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Vol 29: The Classics - Part 2
I so fully believed
that this was owing to the frequent earthquakes, that I felt
inclined to hurry from below each loose pile. As one might
very easily be deceived in a fact of this kind, I doubted its
accuracy, until ascending Mount Wellington, in Van Die-
men's Land, where earthquakes do not occur ; and there I saw
the summit of the mountain similarly composed and similarly
shattered, but all the blocks appeared as if they had been
hurled into their present position thousands of years ago.
We spent the day on the summit, and I never enjoyed one
more thoroughly. Chile, bounded by the Andes and the
Pacific, was seen as in a map. The pleasure from the scenery,
in itself beautiful, was heightened by the many reflections
which arose from the mere view of the Campana range with
its lesser parallel ones, and of the broad valley of Quillota
directly intersecting them. Who can avoid wondering at the
force which has upheaved these mountains, and even more
so at the countless ages which it must have required to have
broken through, removed, and levelled whole masses of them?
It is well in this case to call to mind the vast shingle and
sedimentary beds of Patagonia, which, if heaped on the Cor-
dillera, would increase its height by so many thousand feet.
When in that country, I wondered how any mountain-chain
could have supplied such masses, and not have been utterly
obliterated. We must not now reverse the wonder, and doubt
whether all-powerful time can grind down mountains — even
the gigantic Cordillera — into gravel and mud.
The appearance of the Andes was different from that
which I had expected. The lower line pf the snow was of
THE VOYAGE OF THE BEAGLE 275
course horizontal, and to this line the even summits of the
range seemed quite parallel. Only at long intervals, a group
of points or a single cone showed where a volcano had
existed, or does now exist. Hence the range resembled a
great solid wall, surmounted here and there by a tower, and
making a most perfect barrier to the country.
Almost every part of the hill had been drilled by attempts
to open gold-mines: the rage for mining has left scarcely
a spot in Chile unexamined. I spent the evening as before,
talking round the fire with my two companions. The Guasos
of Chile, who correspond to the Gauchos of the Pampas, are,
however, a very different set of beings. Chile is the more
civilized of the two countries, and the inhabitants, in conse-
quence, have lost much individual character. Gradations in
rank are much more strongly marked: the Guaso does not
by any means consider every man his equal ; and I was quite
surprised to find that my companions did not like to eat at
the same time with myself. This feeling of inequality is a
necessary consequence of the existence of an aristocracy of
wealth. It is said that some few of the greater landowners
possess from five to ten thousand pounds sterling per annum :
an inequality of riches which I believe is not met with in
any of the cattle-breeding countries eastward of the Andes.
A traveller does not here meet that unbounded hospitality
which refuses all payment, but yet is so kindly offered that
no scruples can be raised in accepting it. Almost every house
in Chile will receive you for the night, but a trifle is expected
to be given in the morning; even a rich man will accept two
or three shillings. The Gaucho, although he may be a cut-
throat, is a gentleman; the Guaso is in few respects better,
but at the same time a vulgar, ordinary fellow. The two men,
although employed much in the same manner, are different in
their habits and attire; and the peculiarities of each are
universal in their respective countries. The Gaucho seems
part of his horse, and scorns to exert himself except when
on his back : the Guaso may be hired to work as a labourer in
the fields. The former lives entirely on animal food ; the latter
almost wholly on vegetable. We do not here see the white
boots, the broad drawers and scarlet chilipa; the picturesque
costume of the Pampas. Here, common trousers are pro-
276 CHARLES DARWIN
tected by black and green worsted leggings. The poncho,
however, is common to both. The chief pride of the Guaso
lies in his spurs, which are absurdly large. I measured one
which was six inches in the diameter of the rowel, and the
rowel itself contained upwards of thirty points. The stirrups
are on the same scale, each consisting of a square, carved
block of wood, hollowed out, yet weighing three or four
pounds. The Guaso is perhaps more expert with the lazo
than the Gaucho; but, from the nature of the country, he
does not know the use of the bolas.
August 18th. — We descended the mountain, and passed
some beautiful little spots, with rivulets and fine trees. Hav-
ing slept at the same hacienda as before, we rode during the
two succeeding days up the valley, and passed through Quil-
lota, which is more like a collection of nursery-gardens than
a town. The orchards were beautiful, presenting one mass
of peach-blossoms. I saw, also, in one or two places the
date-palm ; it is a most stately tree ; and I should think a
group of them in their native Asiatic or African deserts must
be superb. We passed likewise San Felipe, a pretty strag-
gling town like Quillota. The valley in this part expands into
one of those great bays or plains, reaching to the foot of the
Cordillera, which have been mentioned as forming so curious
a part of the scenery of Chile. In the evening we reached
the mines of Jajuel, situated in a ravine at the flank of the
great chain. I stayed here five days. My host, the superin-
tendent of the mine, was a shrewd but rather ignorant Cor-
nish miner. He had married a Spanish woman, and did not
mean to return home ; but his admiration for the mines of
Cornwall remained unbounded. Amongst many other ques-
tions, he asked me, " Now that George Rex is dead, how
many more of the family of Rexes are yet alive? " This Rex
certainly must be a relation of the great author Finis, who
wrote all books !
These mines are of copper, and the ore is all shipped to
Swansea, to be smelted. Hence the mines have an aspect
singularly quiet, as compared to those in England : here no
smoke, furnaces, or great steam-engines, disturb the solitude
of the surrounding mountains.
The Chilian government, or rather the old Spanish law.
THE VOYAGE OF THE BEAGLE 277
encourages by every method the searching for mines. The
discoverer may work a mine on any ground, by paying five
shillings; and before paying this he may try, even in the
garden of another man, for twenty days.
It is now well known that the Chilian method of mining
is the cheapest. My host says that the two principal improve-
ments introduced by foreigners have been, first, reducing by
previous roasting the copper pyrites — which, being the com-
mon ore in Cornwall, the English miners were astounded on
their arrival to find thrown away as useless : secondly, stamp-
ing and washing the scoriae from the old furnaces — by which
process particles of metal are recovered in abundance. I have
actually seen mules carrying to the coast, for transportation
to England, a cargo of such cinders. But the first case is
much the most curious. The Chilian miners were so con-
vinced that copper pyrites contained not a particle of copper,
that they laughed at the Englishmen for their ignorance,
who laughed in turn, and bought their richest veins for a
few dollars. It is very odd that, in a country where mining
had been extensively carried on for many years, so simple a
process as gently roasting the ore to expel the sulphur pre-
vious to smelting it, had never been discovered. A few im-
provements have likewise been introduced in some of the
simple machinery; but even to the present day, water is
removed from some mines by men carrying it up the shaft in
leathern bags !
The labouring men work very hard. They have little time
allowed for their meals, and during summer and winter they
begin when it is light, and leave off at dark. They are paid
one pound sterling a month, and their food is given them:
this for breakfast consists of sixteen figs and two small loaves
of bread ; for dinner, boiled beans ; for supper, broken roasted
wheat grain. They scarcely ever taste meat; as, with the
twelve pounds per annum, they have to clothe themselves, and
support their families. The miners who work in the mine
itself have twenty-five shillings per month, and are allowed
a little charqui. But these men come down from their bleak
habitations only once in every fortnight or three weeks.
During my stay here I thoroughly enjoyed scrambling
about these huge mountains. The geology, as might have
VOL. XXIX— R HC
278 CHARLES DARWIN
been expected, was very interesting. The shattered and
baked rocks, traversed by innumerable dykes of greenstone,
showed what commotions had formerly taken place. The
scenery was much the same as that near the Bell of Quil-
lota — dry barren mountains, dotted at intervals by bushes
with a scanty foliage. The cactuses, or rather opuntias,
were here very numerous. I measured one of a spherical
figure, which, including the spines, was six feet and four
inches in circumference. The height of the common cylin-
drical, branching kind, is from twelve to fifteen feet, and
the girth (with spines) of the branches between three and
four feet.
A heavy fall of snow on the mountains prevented me,
during the last two days, from making some interesting
excursions. I attempted to reach a lake which the inhab-
itants, from some unaccountable reason, believe to be an arm
of the sea. During a very dry season, it was proposed to
attempt cutting a channel from it for the sake of the water,
but the padre, after a consultation, declared it was too dan-
gerous, as all Chile would be inundated, if, as generally
supposed, the lake was connected with the Pacific. We
ascended to a great height, but becoming involved in the
snow-drifts failed in reaching this wonderful lake, and had
some difficulty in returning. I thought we should have lost
our horses; for there was no means of guessing how deep
the drifts were, and the animals, when led, could only move
by jumping. The black sky showed that a fresh snow-
storm was gathering, and we therefore were not a little glad
when we escaped. By the time we reached the base the
storm commenced, and it was lucky for us that this did not
happen three hours earlier in the day.
August 26th. — We left Jajuel and again crossed the basin
of San Felipe. The day was truly Chilian : glaringly bright,
and the atmosphere quite clear. The thick and uniform
covering of newly fallen snow rendered the view of the vol-
cano of Aconcagua and the main chain quite glorious. We
were now on the road to Santiago, the capital of Chile. We
crossed the Cerro del Talguen, and slept at a little rancho.
The host, talking about the state of Chile as compared to
other countries, was very humble: " Some see with two eyes,
THE VOYAGE OF THE BEAGLE 279
and some with one, but for my part I do not think that Chile
sees with any."
August 27th. — After crossing many low hills we descended
into the small land-locked plain of Guitron. In the basins,
such as this one, which are elevated from one thousand to
two thousand feet above the sea, two species of acacia, which
are stunted in their forms, and stand wide apart from each
other, grow in large numbers. These trees are never found
near the sea-coast; and this gives another characteristic
feature to the scenery of these basins. We crossed a low
ridge which separates Guitron from the great plain on which
Santiago stands. The view was here pre-eminently striking:
the dead level surface, covered in parts by woods of acacia,
and with the city in the distance, abutting horizontally
against the base of the Andes, whose snowy peaks were
bright with the evening sun. At the first glance of this
view, it was quite evident that the plain represented the
extent of a former inland sea. As soon as we gained the
level road we pushed our horses into a gallop, and reached
the city before it was dark.
I stayed a week in Santiago, and enjoyed myself very
much. In the morning I rode to various places on the plain,
and in the evening dined with several of the English mer-
chants, whose hospitality at this place is well known. A
never-failing source of pleasure was to ascend the little
hillock of rock (St. Lucia) which projects in the middle of
the city. The scenery certainly is most striking, and, as I
have said, very peculiar. I am informed that this same
character is common to the cities on the great Mexican
platform. Of the town I have nothing to say in detail: it is
not so fine or so large as Buenos Ayres, but is built after the
same model. I arrived here by a circuit to the north; so I
resolved to return to Valparaiso by a rather longer excur-
sion to the south of the direct road.
September 5th. — By the middle of the day we arrived at
one of the suspension bridges, made of hide, which cross the
t Maypu, a large turbulent river a few leagues southward of
Santiago. These bridges are very poor affairs. The road,
following the curvature of the suspending ropes, is made of
bundles of sticks placed close together. It was full of holes,
280 CHARLES DARWIN
and oscillated rather fearfully, even with the weight of a
man leading his horse. In the evening we reached a com-
fortable farm-house, where there were several very pretty
senoritas. They were much horrified at my having entered
one of their churches out of mere curiosity. They asked
me, " Why do you not become a Christian — for our religion
is certain ? " I assured them I was a sort of Christian ; but
they would not hear of it — appealing to my own words, " Do
not your padres, your very bishops, marry? " The absurdity
of a bishop having a wife particularly struck them: they
scarcely knew whether to be most amused or horror-struck
at such an enormity.
6th. — We proceeded due south, and slept at Rancagua.
The road passed over the level but narrow plain, bounded on
one side by lofty hills, and on the other by the Cordillera.
The next day we turned up the valley of the Rio Cachapual,
in which the hot-baths of Cauquenes, long celebrated for
their medicinal properties, are situated. The suspension
bridges, in the less frequented parts, ar generally taken down
during the winter when the rivers are low. Such was the
case in this valley, and we were therefore obliged to cross
the stream on horseback. This is rather disagreeable, for
the foaming water, though not deep, rushes so quickly over
the bed of large rounded stones, that one's head becomes
quite confused, and it is difficult even to perceive whether
the horse is moving onward or standing still. In summer,
when the snow melts, the torrents are quite impassable ; their
strength and fury are then extremely great, as might be
plainly seen by the marks which they had left. We reached
the baths in the evening, and stayed there five days, being
confined the two last by heavy rain. The buildings consist
of a square of miserable little hovels, each with a single table
and bench. They are situated in a narrow deep valley just
without the central Cordillera. It is a quiet, solitary spot,
with a good deal of wild beauty.
The mineral springs of Cauquenes burst forth on a line of
dislocation, crossing a mass of stratified rock, the whole
of which betrays the action of heat. A considerable quantity
of gas is continually escaping from the same orifices with
the water. Though the springs are only a few yards apart,
THE VOYAGE OF THE BEAGLE 281
they have very different temperature; and this appears to be
the result of an unequal mixture of cold water: for those
with the lowest temperature have scarcely any mineral taste.
After the great earthquake of 1822 the springs ceased, and
the water did not return for nearly a year. They were also
much affected by the earthquake of 1835; the temperature
being suddenly changed from 118 to 92V It seems probable
that mineral waters rising deep from the bowels of the earth,
would always be more deranged by subterranean disturbances
than those nearer the surface. The man who had charge of
the baths assured me that in summer the water is hotter and
more plentiful than in winter. The former circumstance I
should have expected, from the less mixture, during the dry
season, of cold water; but the latter statement appears very
strange and contradictory. The periodical increase during
the summer, when rain never falls, can, I think, only be
accounted for by the melting of the snow: yet the mountains
which are covered by snow during that season, are three or
four leagues distant from the springs. I have no reason to
doubt the accuracy of my informer, who, having lived on
the spot for several years, ought to be well acquainted with
the circumstance, — which, if true, certainly is very curious:
for we must suppose that the snow-water, being conducted
through porous strata to the regions of heat, is again thrown
up to the surface by the line of dislocated and injected rocks
at Cauquenes; and the regularity of the phenomenon would
seem to indicate that in this district heated rock occurred at
a depth not very great.
One day I rode up the valley to the farthest inhabited
spot. Shortly above that point, the Cachapual divides into
two deep tremendous ravines, which penetrate directly into
the great range. I scrambled up a peaked mountain, prob-
ably more than six thousand feet high. Here, as indeed
everywhere else, scenes of the highest interest presented
themselves. It was by one of these ravines, that Pincheira
entered Chile and ravaged the neighbouring country. This
is the same man whose attack on an estancia at the Rio Negro
I have described. He was a renegade half-caste Spaniard,
who collected a great body of Indians together and estab-
1 Caldcleugh, in Philosoph. Transact, for 1836.
282 CHARLES DARWIN
lished himself oy a stream in the Pampas, which place none
of the forces sent after him could ever discover. From this
point he used to sally forth, and crossing the Cordillera by
passes hitherto unattempted, he ravaged the farm-houses
and drove the cattle to his secret rendezvous. Pincheira was
a capital horseman, and he made all around him equally
good, for he invariably shot any one who hesitated to follow
him. It was against this man, and other wandering Indian
tribes, that Rosas waged the war of extermination.
September 13th. — We left the baths of Cauquenes, and,
rejoining the main road, slept at the Rio Clara. From this
place we rode to the town of San Fernando. Before arriving
there, the last land-locked basin had expanded into a great
plain, which extended so far to the south, that the snowy
summits of the more distant Andes were seen as if above the
horizon of the sea. San Fernando is forty leagues from San-
tiago; and it was my farthest point southward; for we here
turned at right angles towards the coast. We slept at the
gold-mines of Yaquil, which are worked by Mr. Nixon, an
American gentleman, to whose kindness I was much in-
debted during the four days I stayed at his house. The next
morning we rode to the mines, which are situated at the
distance of some leagues, near the summit of a lofty hill. On
the way we had a glimpse of the lake Tagua-tagua, cele-
brated for its floating islands, which have been described by
M. Gay. 2 They are composed of the stalks of various dead
plants intertwined together, and on the surface of which
other living ones take root. Their form is generally circular,
and their thickness from four to six feet, of which the
greater part is immersed in the water. As the wind blows,
they pass from one side of the lake to the other, and often
carry cattle and horses as passengers.
When we arrived at the mine, I was struck by the pale
appearance of many of the men, and inquired from Mr.
Nixon respecting their condition. The mine is 450 feet deep,
and each man brings up about 200 pounds weight of stone.
With this load they have to climb up the alternate notches cut
in the trunks of trees, placed in a zigzag line up the shaft.
2 Annales des Sciences Naturelles, March, 1833. M. Gay, a zealous and
able naturalist, was then occupied in studying every branch of natural
history throughout the kingdom of Chile.
THE VOYAGE OF THE BEAGLE 283
Even beardless young men, eighteen and twenty years old,
with little muscular development of their bodies (they are
quite naked excepting drawers) ascend with this great load
from nearly the same depth. A strong man, who is not
accustomed to this labour, perspires most profusely, with
merely carrying up his own body. With this very severe
labour, they live entirely on boiled beans and bread. They
would prefer having bread alone; but their masters, finding
that they cannot work so hard upon this, treat them like
horses, and make them eat the beans. Their pay is here
rather more than at the mines of Jajuel, being from 24 to 28
shillings per month. They leave the mine only once in three
weeks ; when they stay with their families for two days. One
of the rules of this mine sounds very harsh, but answers
pretty well for the master. The only method of stealing gold
is to secrete pieces of the ore, and take them out as occasion
may offer. Whenever the major-domo finds a lump thus
hidden, its full value is stopped out of the wages of all the
men ; who thus, without they all combine, are obliged to keep
watch over each other.
When the ore is brought to the mill, it is ground into an
impalpable powder; the process of washing removes all the
lighter particles, and amalgamation finally secures the gold-
dust. The washing, when described, sounds a very simple
process; but it is beautiful to see how the exact adaptation of
the current of water to the specific gravity of the gold, so
easily separates the powdered matrix from the metal. The
mud which passes from the mills is collected into pools, where
it subsides, and every now and then is cleared out, and thrown
into a common heap. A great deal of chemical action then
commences, salts of various kinds effloresce on the surface,
and the mass becomes hard. After having been left for a year
or two, and then rewashed, it yields gold; and this process
may be repeated even six or seven times ; but the gold each
time becomes less in quantity, and the intervals required (as
the inhabitants say, to generate the metal) are longer. There
can be no doubt that the chemical action, already mentioned,
each time liberates fresh gold from some combination. The
discovery of a method to effect this before the first grinding,
would without doubt raise the value of gold-ores many fold.
284 CHARLES DARWIN
It is curious to find how the minute particles of gold, being
scattered about and not corroding, at last accumulate in
some quantity. A short time since a few miners, being out of
work, obtained permission to scrape the ground round the
house and mills ; they washed the earth thus got together, and
so procured thirty dollars' worth of gold. This is an exact
counterpart of what takes place in nature. Mountains suffer
degradation and wear away, and with them the metallic veins
which they contain. The hardest rock is worn into impalpa-
ble mud, the ordinary metals oxidate, and both are removed;
but gold, platina, and a few others are nearly indestructible,
and from their weight, sinking to the bottom, are left behind.
After whole mountains have passed through this grinding
mill, and have been washed by the hand of nature, the residue
becomes metalliferous, and man finds it worth his while to
complete the task of separation.
Bad as the above treatment of the miners appears, it is
gladly accepted of by them; for the condition of the labour-
ing agriculturists is much worse. Their wages are lower, and
they live almost exclusively on beans. This poverty must be
chiefly owing to the feudal-like system on which the land is
tilled: the landowner gives a small plot of ground to the
labourer, for building on and cultivating, and in return has
his services (or those of a proxy) for every day of his life,
without any wages. Until a father has a grown-up son, who
can by his labour pay the rent, there is no one, except on
occasional days, to take care of his own patch of ground.
Hence extreme poverty is very common among the labouring
classes in this country.
There are some old Indian ruins in this neighbourhood,
and I was shown one of the perforated stones, which Molina
mentions as being found in many places in considerable
numbers. They are of a circular flattened form, from five to
six inches in diameter, with a hole passing quite through the
centre. It has generally been supposed that they were used
as heads to clubs, although their form does not appear at all
well adapted for that purpose. Burchell 3 states that, some
of the tribes in Southern Africa dig up roots by the aid of a
stick pointed at one end, the force and weight of which are
8 Burchell's Travels, vol. ii. p. 45.
THE VOYAGE OF THE BEAGLE 285
increased by a round stone with a hole in it, into which the
other end is firmly wedged. It appears probable that the
Indians of Chile formerly used some such rude agricultural
instrument.
One day, a German collector in natural history, of the
name of Renous, called, and nearly at the same time an old
Spanish lawyer. I was amused at being told the conversation
which took place between them. Renous speaks Spanish so
well, that the old lawyer mistook him for a Chilian. Renous,
alluding to me, asked him what he thought of the King of
England sending out a collector to their country, to pick up
lizards and beetles, and to break stones? The old gentleman
thought seriously for some time, and then said, " It is not
well, — hay un gato encerrado aqui (there is a cat shut up
here). No man is so rich as to send out people to pick up
such rubbish. I do not like it: if one of us were to go and
do such things in England, do not you think the King of
England would very soon send us out of his country? " And
this old gentleman, from his profession, belongs to the better
informed and more intelligent classes ! Renous himself, two
or three years before, left in a house at San Fernando some
caterpillars, under charge of a girl to feed, that they might
turn into butterflies. This was rumoured through the town,
and at last the padres and governor consulted together, and
agreed it must be some heresy. Accordingly, when Renous
returned, he was arrested.
September ipth. — We left Yaquil, and followed the flat
valley, formed like that of Quillota, in which the Rio Tin-
deridica flows. Even at these few miles south of Santiago
the climate is much damper; in consequence there are fine
tracts of pasturage, which are not irrigated. (20th.) We
followed this valley till it expanded into a great plain, which
reaches from the sea to the mountains west of Rancagua.
We shortly lost all trees and even bushes ; so that the inhabi-
tants are nearly as badly off for firewood as those in the Pam-
pas. Never having heard of these plains, I was much
surprised at meeting with such scenery in Chile. The plains
belong to more than one series of different elevations, and
they are traversed by broad flat-bottomed valleys; both of
which circumstances, as in Patagonia, bespeak the action of
286 CHARLES DARWIN
the sea on gently rising land. In the steep cliffs bordering
these valleys, there are some large caves, which no doubt
were originally formed by the waves: one of these is cele-
brated under the name of Cueva del Obispo ; having formerly
been consecrated. During the day I felt very unwell, and
from that time till the end of October did not recover.
September 22nd. — We continued to pass over green plains
without a tree. The next day we arrived at a house near
Navedad, on the sea-coast, where a rich Haciendero gave us
lodgings. I stayed here the two ensuing days, and although
very unwell, managed to collect from the tertiary formation
some marine shells.
24th. — Our course was now directed towards Valparaiso,
which with great difficulty I reached on the 27th, and was there
confined to my bed till the end of October. During this time
I was an inmate in Mr. Corfield's house, whose kindness to
me I do not know how to express.
I will here add a few observations on some of the animals
and birds of Chile. The Puma, or South American Lion, is
not uncommon. This animal has a wide geographical range ;
being found from the equatorial forests, throughout the
deserts of Patagonia, as far south as the damp and cold
latitudes (53 to 54 ) of Tierra del Fuego. I have seen its
footsteps in the Cordillera of central Chile, at an elevation of
at least 10,000 feet. In La Plata the puma preys chiefly on
deer, ostriches, bizcacha, and other small quadrupeds ; it there
seldom attacks cattle or horses, and most rarely man. In
Chile, however, it destroys many young horses and cattle,
owing probably to the scarcity of other quadrupeds : I heard,
likewise, of two men and a woman who had been thus killed.
It is asserted that the puma always kills its prey by springing
on the shoulders, and then drawing back the head with one
of its paws, until the vertebrae break: I have seen in Pata-
gonia the skeletons of guanacos, with their necks thus
dislocated.
The puma, after eating its fill, covers the carcass with
many large bushes, and lies down to watch it. This habit is
often the cause of its being discovered; for the condors
wheeling in the air every now and then descend to partake
THE VOYAGE OF THE BEAGLE 287
of the feast, and being angrily driven away, rise all together
on the wing. The Chileno Guaso then knows there is a lion
watching his prey — the word is given — and men and dogs
hurry to the chase. Sir F. Head says that a Gaucho in the
Pampas, upon merely seeing some condors wheeling in the
air, cried " A lion ! " I could never myself meet with any one
who pretended to such powers of discrimination. It is as-
serted that, if a puma has once been betrayed by thus watch-
ing the carcass, and has then been hunted, it never resumes
this habit ; but that, having gorged itself, it wanders far away.
The puma is easily killed. In an open country, it is first
entangled with the bolas, then lazoed, and dragged along the
ground till rendered insensible. At Tandeel (south of the
Plata), I was told that within three months one hundred
were thus destroyed. In Chile they are generally driven up
bushes or trees, and are then either shot, or baited to death
by dogs. The dogs employed in this chase belong to a par-
ticular breed, called Leoneros : they are weak, slight animals,
like long-legged terriers, but are born with a particular
instinct for this sport. The puma is described as being very
crafty: when pursued, it often returns on its former track,
and then suddenly niaking a spring on one side, waits there
till the dogs have passed by. It is a very silent animal,
uttering no cry even when wounded, and only rarely during
the breeding season.
Of birds, two species of the genus Pteroptochos (mega-
podius and albicollis of Kittlitz) are perhaps the most con-
spicuous. The former, called by the Chilenos " el Turco,"
is as large as a fieldfare, to which bird it has some alliance ;
but its legs are much longer, tail shorter, and beak stronger :
its colour is a reddish brown. The Turco is not uncommon.
It lives on the ground, sheltered among the thickets which are
scattered over the dry and sterile hills. With its tail erect,
and stilt-like legs, it may be seen every now and then pop-
ping from one bush to another with uncommon quickness.
It really requires little imagination to believe that the bird is
ashamed of itself, and is aware of its most ridiculous figure.
On first seeing it, one is tempted to exclaim, " A vilely stuffed
specimen has escaped from some museum, and has come to
life again ! " It cannot be made to take flight without the
288 CHARLES DARWIN
greatest trouble, nor does it run, but only hops. The various
loud cries which it utters when concealed amongst the bushes,
are as strange as its appearance. It is said to build its
nest in a deep hole beneath the ground. I dissected several
specimens: the gizzard, which was very muscular, contained
beetles, vegetable fibres, and pebbles. From this character,
from the length of its legs, scratching feet, membranous
covering to the nostrils, short and arched wings, this bird
seems in a certain degree to connect the thrushes with the
gallinaceous order.
The second species (or P. albicollis) is allied to the first
in its general form. It is called Tapacolo, or " cover your
posterior ;" and well does the shameless little bird deserve its
name; for it carries its tail more than erect, that is, inclined
backwards towards its head. It is very common, and fre-
quents the bottoms of hedge-rows, and the bushes scattered
over the barren hills, where scarcely another bird can exist.
In its general manner of feeding, of quickly hopping out of
the thickets and back again, in its desire of concealment,
unwillingness to take flight, and nidification, it bears a close
resemblance to the Turco; but its appearance is not quite so
ridiculous. The Tapacolo is very crafty : when frightened by
any person, it will remain motionless at the bottom of a bush,
and will then, after a little while, try with much address to
crawl away on the opposite side. It is also an active bird, and
continually making a noise : these noises are various and
strangely odd; some are like the cooing of doves, others like
the bubbling of water, and many defy all similes. The coun-
try people say it changes its cry five times in the year —
according to some change of season, I suppose. 4
Two species of humming-birds are common; Trochilus
forficatus is found over a space of 2500 miles on the west
coast, from the hot dry country of Lima, to the forests of
Tierra del Fuego — where it may be seen flitting about in
snow-storms. In the wooded island of Chiloe, which has an
* It is a remarkable fact, that Molina, though describing in detail all the
birds and animals of Chile, never once mentions this genus, the species
of which are so common, and so remarkable in their habits. Was he at
a loss how to classify them, and did he consequently think that silence
was the more prudent course? It is one more instance of the frequency
of omissions by authors, on those very subjects where it might have been
least expected.
THE VOYAGE OF THE BEAGLE 289
extremely humid climate, this little bird, skipping from side
to side amidst the dripping foliage, is perhaps more abundant
than almost any other kind. I opened the stomachs of several
specimens, shot in different parts of the continent, and in all,
remains of insects were as numerous as in the stomach of a
creeper. When this species migrates in the summer south-
ward, it is replaced by the arrival of another species coming
from the north. This second kind (Trochilus gigas) is a
very large bird for the delicate family to which it belongs:
when on the wing its appearance is singular. Like others
of the genus, it moves from place to place with a rapidity
which may be compared to that of Syrphus amongst flies,
and Sphinx among moths ; but whilst hovering over a flower,
it flaps its wings with a very slow and powerful movement,
totally different from that vibratory one common to most of
the species, which produces the humming noise. I never saw
any other bird where the force of its wings appeared (as in a
butterfly) so powerful in proportion to the weight of its body.
When hovering by a flower, its tail is constantly expanded
and shut like a fan, the body being kept in a nearly vertical
position. This action appears to steady and support the bird,
between the slow 'movements of its wings. Although flying
from flower to flower in search of food, its stomach generally
contained abundant remains of insects, which I suspect are
much more the object of its search than honey. The note of
this species, like that of nearly the whole family, is extremely
shrill.
vol. xxix— -j hc
CHAPTER XIII
Chiloe and Chonos Islands
Chiloe — General Aspect — Boat Excursion — Native Indians — Castro —
Tame Fox — Ascend San Pedro — Chonos Archipelago — Peninsula
of Tres Montes — Granitic Range — Boat-wrecked Sailors — Low's
Harbour — Wild Potato — Formation of Peat — Myopotamus, Otter
and Mice — Cheucau and Barking-bird — Opetiorhynchus — Singular
Character of Ornithology—Petrels.
71 TOVEMBER ioth.—Tht Beagle sailed from Valparaiso
/ y to the south, for the purpose of surveying the south-
ern part of Chile, the island of Chiloe, and the broken
land called the Chonos Archipelago, as far south as the
Peninsula of Tres Montes. On the 21st we anchored in the
bay of S. Carlos, the capital of Chiloe.
This island is about ninety miles long, with a breadth of
rather less than thirty. The land is hilly, but not mountain-
ous, and is covered by one great forest, except where a few
green patches have been cleared round the thatched cottages.
From a distance the view somewhat resembles that of Tierra
del Fuego ; but the woods, when seen nearer, are incompara-
bly more beautiful. Many kinds of fine evergreen trees, and
plants with a tropical character, here take the place of the
gloomy beech of the southern shores. In winter the climate
is detestable, and in summer it is only a little better. I should
think there are few parts of the world, within the temperate
regions, where so much rain falls. The winds are very bois-
terous, and the sky almost always clouded : to have a week of
fine weather is something wonderful. It is even difficult to
get a single glimpse of the Cordillera : during our first visit,
once only the volcano of Osorno stood out in bold relief, and
that was before sunrise; it was curious to watch, as the sun
rose, the outline gradually fading away in the glare of the
eastern sky.
The inhabitants, from their complexion and low stature,
290
THE VOYAGE OF THE BEAGLE 291
appear to have three-fourths of Indian blood in their veins.
They are an humble, quiet, industrious set of men. Although
the fertile soil, resulting from the decomposition of the vol-
canic rocks, supports a rank vegetation, yet the climate is not
favourable to any production which requires much sunshine
to ripen it. There is very little pasture for the larger quad-
rupeds; and in consequence, the staple articles of food are
pigs, potatoes, and fish. The people all dress in strong
woollen garments, which each family makes for itself, and
dyes with indigo of a dark blue colour. The arts, however,
are in the rudest state; — as may be seen in their strange
fashion of ploughing, their method of spinning, grinding
corn, and in the construction of their boats. The forests are
so impenetrable, that the land is nowhere cultivated except
near the coast and on the adjoining islets. Even where paths
exist, they are scarcely passable from the soft and swampy
state of the soil. The inhabitants, like those of Tierra del
Fuego, move about chiefly on the beach or in boats. Although
with plenty to eat, the people are very poor: there is no
demand for labour, and consequently the lower orders cannot
scrape together money sufficient to purchase even the smallest
luxuries. There is also a great deficiency of a circulating
medium. I have seen a man bringing on his back a bag of
charcoal, with which to buy some trifle, and another carrying
a plank to exchange for a bottle of wine. Hence every trades-
man must also be a merchant, and again sell the goods which
he takes in exchange.
November 24th. — The yawl and whale-boat were sent under
the command of Mr. (now Captain) Sulivan, to survey the
eastern or inland coast of Chiloe; and with orders to meet
the Beagle at the southern extremity of the island ; to which
point she would proceed by the outside, so as thus to cir-
cumnavigate the whole. I accompanied this expedition, but
instead of going in the boats the first day, I hired horses to
take me to Chacao, at the northern extremity of the island.
The road followed the coast; every now and then crossing
promontories covered by fine forests. In these shaded paths
it is absolutely necessary that the whole road should be made
of logs of wood, which are squared and placed by the side of
each other. From the rays of the sun never penetrating the
292 CHARLES DARWIN
evergreen foliage, the ground is so damp and soft, that except
by this means neither man nor horse would be able to pass
along. I arrived at the village of Chacao shortly after the
tents belonging to the boats were pitched for the night.
The land in this neighbourhood has been extensively
cleared, and there were many quiet and most picturesque
nooks in the forest. Chacao was formerly the principal port
in the island ; but many vessels having been lost, owing to the
dangerous currents and rocks in the straits, the Spanish gov-
ernment burnt the church, and thus arbitrarily compelled the
greater number of inhabitants to migrate to S. Carlos. We
had not long bivouacked, before the barefooted son of the
governor came down to reconnoitre us. Seeing the English
flag hoisted at the yawl's mast-head, he asked with the utmost
indifference, whether it was always to fly at Chacao. In sev-
eral places the inhabitants were much astonished at the
appearance of men-of-war's boats, and hoped and believed
it was the forerunner of a Spanish fleet, coming to recover
the island from the patriot government of Chile. All the
men in power, however, had been informed of our intended
visit, and were exceedingly civil. While we were eating our
supper, the governor paid us a visit. He had been a lieuten-
ant-colonel in the Spanish service, but now was miserably
poor. He gave us two sheep, and accepted in return two cot-
ton handkerchiefs, some brass trinkets, and a little tobacco.
25th. — Torrents of rain: we managed, however, to run
down the coast as far as Huapi-lenou. The whole of this
eastern side of Chiloe has one aspect ; it is a plain, broken by
valleys and divided into little islands, and the whole thickly
covered with one impervious blackish-green forest. On the
margins there are some cleared spaces, surrounding the high-
roofed cottages.
26th. — The day rose splendidly clear. The volcano of
Orsono was spouting out volumes of smoke. This most
beautiful mountain, formed like a perfect cone, and white
with snow, stands out in front of the Cordillera. Another
great volcano, with a saddle-shaped summit, also emitted
from its immense crater little jets of steam. Subsequently
we saw the lofty-peaked Corcovado — well deserving the name
of " el famoso Corcovado." Thus we beheld, from one point
THE VOYAGE OF THE BEAGLE 293
of view, three great active volcanoes, each about seven thou-
sand feet high. In addition to this, far to the south, there
were other lofty cones covered with snow, which, although
not known to be active, must be in their origin volcanic.
The line of the Andes is not, in this neighbourhood, nearly
so elevated as in Chile; neither does it appear to form so
perfect a barrier between the regions of the earth. This
great range, although running in a straight north and south
line, owing to an optical deception, always appeared more or
less curved; for the lines drawn from each peak to the
beholder's eye, necessarily converged like the radii of a
semicircle, and as it was not possible (owing to the clearness
of the atmosphere and the absence of all intermediate ob-
jects) to judge how far distant the farthest peaks were off,
they appeared to stand in a flattish semicircle.
Landing at midday, we saw a family of pure Indian extrac-
tion. The father was singularly like York Minster ; and some
of the younger boys, with their ruddy complexions, might
have been mistaken for Pampas Indians. Everything I have
seen, convinces me of the close connexion of the different
American tribes, who nevertheless speak distinct languages.
This party could muster but little Spanish, and talked to each
other in their own tongue. It is a pleasant thing to see the
aborigines advanced to the same degree of civilization, how-
ever low that may be, which their white conquerors have
attained. More to the south we saw many pure Indians:
indeed, all the inhabitants of some of the islets retain their
Indian surnames. In the census of 1832, there were in Chiloe
and its dependencies forty-two thousand souls ; the greater
number of these appear to be of mixed blood. Eleven thou-
sand retain their Indian surnames, but it is probable that not
nearly all of these are of a pure breed. Their manner of life
is the same with that of the other poor inhabitants, and they
are all Christians; but it is said that they yet retain some
strange superstitious ceremonies, and that they pretend to
hold communication with the devil in certain caves. For-
merly, every one convicted of this offence was sent to the
Inquisition at Lima. Many of the inhabitants who are not
included in the eleven thousand with Indian surnames, can-
not be distinguished by their appearance from Indians.
294 CHARLES DARWIN
Gomez, the governor of Lemuy, is descended from noblemtn
of Spain on both sides; but by constant intermarriages with
the natives the present man is an Indian. On the other hand,
the governor of Quinchao boasts much of his purely kept
Spanish blood.
We reached at night a beautiful little cove, north of the
island of Caucahue. The people here complained of want of
land. This is partly owing to their own negligence in not
clearing the woods, and partly to restrictions by the govern-
ment, which makes it necessary, before buying ever so small
a piece, to pay two shillings to the surveyor for measuring
each quadra (150 yards square), together with whatever
price he fixes for the value of the land. After his valuation,
the land must be put up three times to auction, and if no one
bids more, the purchaser can have it at that rate. All these
exactions must be a serious check to clearing the ground,
where the inhabitants are so extremely poor. In most coun-
tries, forests are removed without much difficulty by the aid
of fire; but in Chiloe, from the damp nature of the climate,
and the sort of trees, it is necessary first to cut them down.
This is a heavy drawback to the prosperity of Chiloe. In the
time of the Spaniards the Indians could not hold land ; and a
family, after having cleared a piece of ground, might be
driven away, and the property seized by the government.
The Chilian authorities are now performing an act of justice
by making retribution to these poor Indians, giving to each
man, according to his grade of life, a certain portion of land.
The value of uncleared ground is very little. The govern-
ment gave Mr. Douglas (the present surveyor, who informed
me of these circumstances) eight and a half square miles of
forest near S. Carlos, in lieu of a debt; and this he sold for
350 dollars, or about 70/. sterling.
The two succeeding days were fine, and at night we reached
the island of Quinchao. This neighbourhood is the most cul-
tivated part of the Archipelago; for a broad strip of land on
the coast of the main island, as well as on many of the smaller
adjoining ones, is almost completely cleared. Some of the
farmhouses seemed very comfortable. I was curious to
ascertain how rich any of these people might be, but Mr.
Douglas says that no one can be considered as possessing a
THE VOYAGE OF THE BEAGLE 295
regular income. One of the richest land-owners might pos-
sibly accumulate, in a long industrious life, as much as iooo/.
sterling ; but should this happen, it would all be stowed away
in some secret corner, for it is the custom of almost every
family to have a jar or treasure-chest buried in the ground.
November 30th. — Early on Sunday morning we reached
Castro, the ancient capital of Chiloe, but now a most forlorn
and deserted place. The usual quadrangular arrangement
of Spanish towns could be traced, but the streets and plaza
were coated with fine green turf, on which sheep were
browsing. The church, which stands in the middle, is entirely
built of plank, and has a picturesque and venerable appear-
ance. The poverty of the place may be conceived from the
fact, that although containing some hundreds of inhabitants,
one of our party was unable anywhere to purchase either a
pound of sugar or an ordinary knife. No individual possessed
either a watch or a clock ; and an old man, who was supposed
to have a good idea of time, was employed to strike the
church bell by guess. The arrival of our boats was a rare
event in this quiet retired corner of the world ; and nearly all
the inhabitants came down to the beach to see us pitch our
tents. They were very civil, and offered us a house ; and one
man even sent us a cask of cider as a present. In the after-
noon we paid our respects to the governor — a quiet old man,
who, in his appearance and manner of life, was scarcely
superior to an English cottager. At night heavy rain set in,
which was hardly sufficient to drive away from our tents the
large circle of lookers-on. An Indian family, who had come
to trade in a canoe from Caylen, bivouacked near us. They
had no shelter during the rain. In the morning I asked a
young Indian, who was wet to the skin, how he had passed
the night. He seemed perfectly content, and answered, " Muy
bien, sefior."
December 1st. — We steered for the island of Lemuy. I
was anxious to examine a reported coal-mine which turned
out to be lignite of little value, in the sandstone (probably
of an ancient tertiary epoch) of which these islands are com-
posed. When we reached Lemuy we had much difficulty in
finding any place to pitch our tents, for it was spring-tide,
and the land was wooded down to the water's edge. In a
296 CHARLES DARWIN
short time we were surrounded by a large group of the nearly
pure Indian inhabitants. They were much surprised at our
arrival, and said one to the other, " This is the reason we
have seen so many parrots lately; the cheucau (an odd red-
breasted little bird, which inhabits the thick forest, and utters
very peculiar noises) has not cried ' beware ' for nothing/'
They were soon anxious for barter. Money was scarcely
worth anything, but their eagerness for tobacco was some-
thing quite extraordinary. After tobacco, indigo came next
in value; then capsicum, old clothes, and gunpowder. The
latter article was required for a very innocent purpose: each
parish has a public musket, and the gunpowder was wanted
for making a noise on their saint or feast days.
The people here live chiefly on shell-fish and potatoes. At
certain seasons they catch also, in " corrales," or hedges
under water, many fish which are left on the mud-banks as
the tide falls. They occasionally possess fowls, sheep, goats,
pigs, horses, and cattle; the order in which they are here
mentioned, expressing their respective numbers. I never
saw anything more obliging and humble than the manners
of these people. They generally began with stating that
they were poor natives of the place, and not Spaniards,
and that they were in sad want of tobacco and other com-
forts. At Caylen, the most southern island, the sailors
bought with a stick of tobacco, of the value of three-half-
pence, two fowls, one of which, the Indian stated, had skin
between its toes, and turned out to be a fine duck; and with
some cotton handkerchiefs, worth three shillings, three sheep
and a large bunch of onions were procured. The yawl at
this place was anchored some way from the shore, and we
had fears for her safety from robbers during the night. Our
pilot, Mr. Douglas, accordingly told the constable of the
district that we always placed sentinels with loaded arms,
and not understanding Spanish, if we saw any person in the
dark, we should assuredly shoot him. The constable, with
much humility, agreed to the perfect propriety of this
arrangement, and promised us that no one should stir out
of his house during that night.
During the four succeeding days we continued sailing
southward. The general features of the country remained
THE VOYAGE OF THE BEAGLE 297
the same, but it was much less thickly inhabited. On the
large island of Tanqui there was scarcely one cleared spot,
the trees on every side extending their branches over the
sea-beach. I one day noticed, growing on the sandstone
cliffs, some very fine plants of the panke (Gunnera scabra),
which somewhat resembles the rhubarb on a gigantic scale.
The inhabitants eat the stalks, which are subacid, and tan
leather with the roots, and prepare a black dye from them.
The leaf is nearly circular, but deeply indented on its mar-
gin. I measured one which was nearly eight feet in diame-
ter, and therefore no less than twenty-four in circumfer-
ence ! The stalk is rather more than a yard high, and each
plant sends out four or five of these enormous leaves, pre-
senting together a very noble appearance.
December 6th. — We reached Caylen, called " el fin del
Cristiandad." In the morning we stopped for a few minutes
at a house on the northern end of Laylec, which was the
extreme point of South American Christendom, and a mis-
erable hovel it was. The latitude is 43 10', which is two
degrees farther south than the Rio Negro on the Atlantic
coast. These extreme Christians were very poor, and, under
the plea of their situation, begged for some tobacco. As a
proof of the poverty of these Indians, I may mention that
shortly before this, we had met a man, who had travelled
three days and a half on foot, and had as many to return,
for the sake of recovering the value of a small axe and a few
fish. How very difficult it must be to buy the smallest article,
when such trouble is taken to recover so small a debt.
In the evening we reached the island of San Pedro, where
we found the Beagle at anchor. In doubling the point, two
of the officers landed to take a round of angles with the
theodolite. A fox (Canis fulvipes), of a kind said to be
peculiar to the island, and very rare in it, and which is a new
species, was sitting on the rocks. He was so intently ab-
sorbed in watching the work of the officers, that I was able,
by quietly walking up behind, to knock him on the head
with my geological hammer. This fox, more curious or
more scientific, but less wise, than the generality of his
brethren, is now mounted in the museum of the Zoological
Society.
298 CHARLES DARWIN
We stayed three days in this harbour, on one of which
Captain Fitz Roy, with a party, attempted to ascend to the
summit of San Pedro. The woods here had rather a differ-
ent appearance from those on the northern part of the island.
The rock, also, being micaceous slate, there was no beach,
but the steep sides dipped directly beneath the water. The
general aspect in consequence was more like that of Tierra
del Fuego than of Chiloe. In vain we tried to gain the
summit: the forest was so impenetrable, that no one who
has not beheld it can imagine so entangled a mass of dying
and dead trunks. I am sure that often, for more than ten
minutes together, our feet never touched the ground, and
we were frequently ten or fifteen feet above it, so that the
seamen as a joke called out the soundings. At other times
we crept one after another on our hands and knees, under
the rotten trunks. In the lower part of the mountain, noble
trees of the Winter's Bark, and a laurel like the sassafras
with fragrant leaves, and others, the names of which I do
not know, were matted together by a trailing bamboo or cane.
Here we were more like fishes struggling in a net than any
other animal. On the higher parts, brushwood takes the
place of larger trees, with here and there a red cedar or an
alerce pine. I was also pleased to see, at an elevation of a
little less than iooo feet, our old friend the southern beech.
They were, however, poor stunted trees; and I should think
that this must be nearly their northern limit. We ultimately
gave up the attempt in despair.
December ioth. — The yawl and whale-boat, with Mr.
Sulivan, proceeded on their survey, but I remained on board
the Beagle, which the next day left San Pedro for the south-
ward. On the 13th we ran into an opening in the southern
part of Guayatecas, or the Chonos Archipelago ; and it was
fortunate we did so, for on the following day a storm, worthy
of Tierra del Fuego, raged with great fury. White massive
clouds were piled up against a dark blue sky, and across them
black ragged sheets of vapour were rapidly driven. The suc-
cessive mountain ranges appeared like dim shadows; and
the setting sun cast on the woodland a yellow gleam, much
like that produced by the flame of spirits of wine. The water
was white with the flying spray, and the wind lulled and
THE VOYAGE OF THE BEAGLE 299
roared again through the rigging: it was an ominous, sub-
lime scene. During a few minutes there was a bright rain-
bow, and it was curious to observe the effect of the spray,
which being carried along the surface of the water, changed
the ordinary semicircle into a circle — a band of prismatic
colours being continued, from both feet of the common arch
across the bay, close to the vessel's side : thus forming a dis-
torted, but very nearly entire ring.
We stayed here three days. The weather continued bad:
but this did not much signify, for the surface of the land
in all these islands is all but impassable. The coast is so
very rugged that to attempt to walk in that direction re-
quires continued scrambling up and down over the sharp
rocks of mica-slate ; and as for the woods, our faces, hands,
and shin-bones all bore witness to the maltreatment we
received, in merely attempting to penetrate their forbidden
recesses.
December 18th. — We stood out to sea. On the 20th we
bade farewell to the south, and with a fair wind turned the
ship's head northward. From Cape Tres Montes we sailed
pleasantly along, the lofty weather-beaten coast, which is
remarkable for the bold outline of its hills, and the thick
covering of forest even on the almost precipitous flanks. The
next day a harbour was discovered, which on this dangerous
coast might be of great service to a distressed vessel. It
can easily be recognized by a hill 1600 feet high, which is
even more perfectly conical than the famous sugar-loaf at
Rio de Janeiro. The next day, after anchoring, I succeeded
in reaching the summit of this hill. It was a laborious under-
taking, for the sides were so steep that in some parts it was
necessary to use the trees as ladders. There were also several
extensive brakes of the Fuchsia, covered with its beautiful
drooping flowers, but very difficult to crawl through. In
these wild countries it gives much delight to gain the summit
of any mountain. There is an indefinite expectation of seeing
something very strange, which, however often it may be
balked, never failed with me to recur on each successive
attempt. Every one must know the feeling of triumph and
pride which a grand view from a height communicates to the
mind. In these little frequented countries there is also joined
300 CHARLES DARWIN
to it some vanity, that you perhaps are the first man who ever
stood on this pinnacle or admired this view.
A strong desire is always felt to ascertain whether any
human being has previously visited an unfrequented spot.
A bit of wood with a nail in it, is picked up and studied as
if it were covered with hieroglyphics. Possessed with this
feeling, I was much interested by finding, on a wild part of
the coast, a bed made of grass beneath a ledge of rock. Close
by it there had been a fire, and the man had used an axe.
The fire, bed, and situation showed the dexterity of an Indian;
but he could scarcely have been an Indian, for the race is
in this part extinct, owing to the Catholic desire of making
at one blow Christians and Slaves. I had at the time some
misgivings that the solitary man who had made his bed on
this wild spot, must have been some poor shipwrecked sailor,
who, in trying to travel up the coast, had here laid himself
down for his dreary night.
December 28th. — The weather continued very bad, but it
at last permitted us to proceed with the survey. The time
hung heavy on our hands, as it always did when we were
delayed from day to day by successive gales of wind. In
the evening another harbour was discovered, where we
anchored. Directly afterwards a man was seen waving a
shirt, and a boat was sent which brought back two seamen.
A party of six had run away from an American whaling
vessel, and had landed a little to the southward in a boat,
which was shortly afterwards knocked to pieces by the surf.
They had now been wandering up and down the coast for
fifteen months, without knowing which way to go, or where
they were. What a singular piece of good fortune it was
that this harbour was now discovered ! Had it not been for
this one chance, they might have wandered till they had
grown old men, and at last have perished on this wild coast.
Their sufferings had been very great, and one of their party
had lost his life by falling from the cliffs. They were some-
times obliged to separate in search of food, and this explained
the bed of the solitary man. Considering what they had
undergone, I think they had kept a very good reckoning of
time, for they had lost only four days.
December 30th. — We anchored in a snug little cove at the
THE VOYAGE OF THE BEAGLE 301
foot of some high hills, near the northern extremity of Tres
Montes. After breakfast the next morning, a party ascended
one of these mountains, which was 2400 feet high. The
scenery was remarkable. The chief part of the range was
composed of grand, solid, abrupt masses of granite, which
appeared as if they had been coeval with the beginning of
the world. The granite was capped with mica-slate, and this
in the lapse of ages had been worn into strange finger-
shaped points. These two formations, thus differing in their
outlines, agree in being almost destitute of vegetation. This
barrenness had to our eyes a strange appearance, from having
been so long accustomed to the sight of an almost universal
forest of dark-green trees. I took much delight in examining
the structure of these mountains. The complicated and lofty
ranges bore a noble aspect of durability — equally profitless,
however, to man and to all other animals. Granite to the
geologist is classic ground : from its widespread limits, and its
beautiful and compact texture, few rocks have been more
anciently recognised. Granite has given rise, perhaps, to
more discussion concerning its origin than any other forma-
tion. We generally see it constituting the fundamental rock,
and, however formed, we know it is the deepest layer in the
crust of this globe to which man has penetrated. The limit
of man's knowledge in any subject possesses a high interest,
which is perhaps increased by its close neighbourhood to the
realms of imagination.
January 1st, 1835. — The new year is ushered in with the
ceremonies proper to it in these regions. She lays out no
false hopes: a heavy north-western gale, with steady rain,
bespeaks the rising year. Thank God, we are not destined
here to see the end of it, but hope then to be in the Pacific
Ocean, where a blue sky tells one there is a heaven, — a some-
thing beyond the clouds above our heads.
The north-west winds prevailing for the next four days,
we only managed to cross a great bay, and then anchored in
another secure harbour. I accompanied the Captain in a
boat to the head of a deep creek. On the way the number of
seals which we saw was quite astonishing: every bit of flat
rock, and parts of the beach, were covered with them. They
appeared to be of a loving disposition, and lay huddled to-
302 CHARLES DARWIN
gether, fast asleep, like so many pigs; but even pigs would
have been ashamed of their dirt, and of the foul smell which
came from them. Each herd was watched by the patient but
inauspicious eyes of the turkey-buzzard. This disgusting bird,
with its bald scarlet head, formed to wallow in putridity, is
very common on the west coast, and their attendance on the
seals shows on what they rely for their food. We found the
water (probably only that of the surface) nearly fresh: this
was caused by the number of torrents which, in the form
of cascades, came tumbling over the bold granite mountains
into the sea. The fresh water attracts the fish, and these
bring many terns, gulls, and two kinds of cormorant. We
saw also a pair of the beautiful black-necked swans, and
several small sea-otters, the fur of which is held in such
high estimation. In returning, we were again amused by the
impetuous manner in which the heap of seals, old and young,
tumbled into the water as the boat passed. They did not
remain long under water, but rising, followed us with out-
stretched necks, expressing great wonder and curiosity.
yth. — Having run up the coast, we anchored near the
northern end of the Chonos Archipelago, in Low's Llarbour,
where we remained a week. The islands were here, as in
Chiloe, composed of a stratified, soft, littoral deposit; and
the vegetation in consequence was beautifully luxuriant. The
woods came down to the sea-beach, just in the manner of
an evergreen shrubbery over a gravel walk. We also enjoyed
from the anchorage a splendid view of four great snowy
cones of the Cordillera, including " el f amoso Corcovado ; "
the range itself had in this latitude so little height, that few
parts of it appeared above the tops of the neighbouring
islets. We found here a party of five men from Caylen, " el
fin del Cristiandad," who had most adventurously crossed in
their miserable boat-canoe, for the purpose of fishing, the
open space of sea which separates Chonos from Chiloe. These
islands will, in all probability, in a short time become peopled
like those adjoining the coast of Chiloe.
The wild potato grows on these islands in great abundance,
on the sandy, shelly soil near the sea-beach. The tallest
plant was four feet in height. The tubers were generally
THE VOYAGE OF THE BEAGLE 303
email, but I found one, of an oval shape, two inches in
diameter : they resembled in every respect, and had the same
smell as English potatoes ; but when boiled they shrunk much,
and were watery and insipid, without any bitter taste. They
are undoubtedly here indigenous: they grow as far south,
according to Mr. Low, as lat. 50 , and are called Aquinas by
the wild Indians of that part: the Chilotan Indians have a
different name for them. Professor Henslow, who has ex-
amined the dried specimens which I brought home, says that
they are the same with those described by Mr. Sabine 1 from
Valparaiso, but that they form a variety which by some
botanists has been considered as specifically distinct. It is
remarkable that the same plant should be found on the sterile
mountains of central Chile, where a drop of rain does not
fall for more than six months, and within the damp forests
of these southern islands.
In the central parts of the Chonos Archipelago (lat. 45°),
the forest has very much the same character with that along
the whole west coast, for 600 miles southward to Cape Horn.
The arborescent grass of Chiloe is not found here ; while the
beech of Tierra del Fuego grows to a good size, and forms a
considerable proportion of the wood; not, however, in the
same exclusive manner as it does farther southward. Crypto-
gamic plants here find a most congenial climate. In the Strait
of Magellan, as I have before remarked, the country appears
too cold and wet to allow of their arriving at perfection ; but
in these islands, within the forest, the number of species and
great abundance of mosses, lichens, and small ferns, is quite
extraordinary.' In Tierra del Fuego trees grow only on the
hillsides; every level piece of land being invariably covered
by a thick bed of peat; but in Chiloe flat land supports the
most luxuriant forests. Here, within the Chonos Archipel-
ago, the nature of the climate more closely approaches that
1 Horticultural Transact., vol. v. p. 249. Mr. Caldcleugh sent home
two tubers, which, being well manured, even the first season produced
numerous potatoes and an abundance of leaves. See Humboldt's interest-
ing discussion on this plant, which it appears was unknown in Mexico, —
in Polit. Essay on New Spain, book iv. chap. ix.
2 By sweeping with my insect-net, I procured from these situations a
considerable number of minute insects, of the family of Staphylinidae, and
others allied to Pselaphus, and minute Hymenoptera. But the most char-
acteristic family in number, both of individuals and species, throughout
the more open parts of Chiloe and Chonos is that of the Telephoridae.
304 CHARLES DARWIN
of Tierra del Fuego than that of northern Chiloe; for every
patch of level ground is covered by two species of plants
(Astelia pumila and Donatia magellanica), which by their
joint decay compose a thick bed of elastic peat.
In Tierra del Fuego, above the region of woodland, the
former of these eminently sociable plants is the chief agent
in the production of peat. Fresh leaves are always succeed-
ing one to the other round the central tap-root; the lower
ones soon decay, and in tracing a root downwards in the peat,
the leaves, yet holding their place, can be observed passing
through every stage of decomposition, till the whole becomes
blended in one confused mass. The Astelia is assisted by a
few other plants, — here and there a small creeping Myrtus
(M. nummularia), with a woody stem like our cranberry and
with a sweet berry, — an Empetrum (E. rubrum), like our
heath, — a rush (Juncus grandiflorus), are nearly the only
ones that grow on the swampy surface. These plants, though
possessing a very close general resemblance to the English
species of the same genera, are different. In the more level
parts of the country, the surface of the peat is broken up into
little pools of water, which stand at different heights, and
appear as if artificially excavated. Small streams of water,
flowing underground, complete the disorganization of the
vegetable matter, and consolidate the whole.
The climate of the southern part of America appears partic-
ularly favourable to the production of peat. In the Falkland
Islands almost every kind of plant, even the coarse grass
which covers the whole surface of the land, becomes con-
verted into this substance: scarcely any situation checks its
growth ; some of the beds are as much as twelve feet thick,
and the lower part becomes so solid when dry, that it will
hardly burn. Although every plant lends its aid, yet in most
parts the Astelia is the most efficient. It is rather a singular
circumstance, as being so very different from what occurs
in Europe, that I nowhere saw moss forming by its decay
any portion of the peat in South America. With respect to
the northern limit, at which the climate allows of that pecul-
iar kind of slow decomposition which is necessary for its
production, I believe that in Chiloe (lat. 41 ° to 42 ), although
there is much swampy ground, no well-characterized peat
THE VOYAGE OF THE BEAGLE 305
occurs: but in the Chonos Islands, three degrees farther
southward, we have seen that it is abundant. On the eastern
coast in La Plata (lat. 35 ) I was told by a Spanish resident
who had visited Ireland, that he had often sought for this
substance, but had never been able to find any. He showed
me, as the nearest approach to it which he had discovered, a
black peaty soil, so penetrated with roots as to allow of an
extremely slow and imperfect combustion.
The zoology of these broken islets of the Chonos Archi-
pelago is, as might have been expected, very poor. Of quad-
rupeds two aquatic kinds are common. The Myopotamus
Coypus (like a beaver, but with a round tail) is well known
from its fine fur, which is an object of trade throughout the
tributaries of La Plata. It here, however, exclusively fre-
quents salt water; which same circumstance has been men-
tioned as sometimes occurring with the great rodent, the
Capybara. A small sea-otter is very numerous; this animal
does not feed exclusively on fish, but, like the seals, draws a
large supply from a small red crab, which swims in shoals
near the surface of the water. Mr. Bynoe saw one in Tierra
del Fuego eating a cuttle-fish ; and at Low's Harbour, another
was killed in the act of carrying to its hole a large volute
shell. At one place I caught in a trap a singular little mouse
(M. brachiotis) ; it appeared common on several of the islets,
but the Chilotans at Low's Harbour said that it was not found
in all. What a succession of chances, 3 or what changes of
level must have been brought into play, thus to spread these
small animals throughout this broken archipelago !
In all parts of Chiloe and Chonos, two very strange birds
occur, which are allied to, and replace, the Turco and Tapa-
colo of central Chile. One is called by the inhabitants
"Cheucau" (Pteroptochos rubecula) : it frequents the most
gloomy and retired spots within the damp forests. Some-
times, although its cry may be heard close at hand, let a per-
son watch ever so attentively he will not see the cheucau; at
8 It is said that some rapacious birds bring their prey alive to their
nests. If so, in the course of centuries, every now and then, one might
escape from the young birds. Some such agency is necessary, to account
for the distribution of the smaller gnawing animals on islands not very
near each other.
306 CHARLES DARWIN
other times, let him stand motionless and the red-breasted
little bird will approach within a few feet in the most familiar
manner. It then busily hops about the entangled mass of
rotting canes and branches, with its little tail cocked upwards.
The cheucau is held in superstitious fear by the Chilotans, on
account of its strange and varied cries. There are three
very distinct cries : one is called " chiduco," and is an omen
of good; another, " huitreu," which is extremely unfavour-
able; and a third, which I have forgotten. These words are
given in imitation of the noises ; and the natives are in some
things absolutely governed by them. The Chilotans assuredly
have chosen a most comical little creature for their prophet.
An allied species, but rather larger, is called by the natives
"Guid-guid" (Pteroptochos Tarnii), and by the English the
barking-bird. This latter name is well given ; for I defy any
one at first to feel certain that a small dog is not yelping
somewhere in the forest. Just as with the cheucau, a person
will sometimes hear the bark close by, but in vain many
endeavour by watching, and with still less chance by beating
the bushes, to see the bird ; yet at other times the guid-guid
fearlessly comes near. Its manner of feeding and its general
habits are very similar to those of the cheucau.
On the coast 4 a small dusky-coloured bird (Opetiorhyn-
chus Patagonicus) is very common. It is remarkable from
its quiet habits; it lives entirely on the sea-beach, like a
sandpiper. Besides these birds only few others inhabit this
broken land. In my rough notes I describe the strange
noises, which, although frequently heard within these gloomy
forests, yet scarcely disturb the general silence. The yelp-
ing of the guid-guid, and the sudden whew-whew of the
cheucau, sometimes come from afar off, and sometimes from
close at hand; the little black wren of Tierra del Fuego oc-
casionally adds its cry; the creeper (Oxyurus) follows the
intruder screaming and twittering; the humming-bird may
be seen every now and then darting from side to side, and
emitting, like an insect, its shrill chirp; lastly, from the top
* I may mention, as a proof of how great a difference there is between the
seasons of the wooded and the open parts of this coast, that on September
20th, in lat. 34°, these birds had young ones in the nest, while among the
Chonos Islands, three months later in the summer, they were only laying,
the difference in latitude between these two places being about 700 miles.
THE VOYAGE OF THE BEAGLE S07
of some lofty tree the indistinct but plaintive note of the
white-tufted tyrant-flycatcher (Myiobius) may be noticed.
From the great preponderance in most countries of certain
common genera of birds, such as the finches, one feels at
first surprised at meeting with the peculiar forms above enu-
merated, as the commonest birds in any district. In central
Chile two of them, namely, the Oxyurus and Scytalopus, oc-
cur, although most rarely. When finding, as in this case,
animals which seem to play so insignificant a part in the great
scheme of nature, one is apt to wonder why they were
created.
But it should always be recollected, that in some other
country perhaps they are essential members of society, or
at some former period may have been so. If America
south of 37 were sunk beneath the waters of the ocean,
these two birds might continue to exist in central Chile for
a long period, but it is very improbable that their numbers
would increase. We should then see a case which must in-
evitably have happened with very many animals.
These southern seas are frequented by several species of
Petrels: the largest kind, Procellaria gigantea, or nelly (que-
brantahuesos, or break-bones, of the Spaniards), is a com-
mon bird, both in the inland channels and on the open sea.
In its habits and manner of flight, there is a very close re-
semblance with the albatross ; and as with the albatross, a
person may watch it for hours together without seeing on
what it feeds. The " break-bones " is, however, a rapacious
bird, for it was observed by some of the officers at Port St.
Antonio chasing a diver, which tried to escape by diving
and flying, but was continually struck down, and at last
killed by a blow on its head. At Port St. Julian these great
petrels were seen killing and devouring young gulls. A sec-
ond species (Puffinus cinereus), which is common to Europe,
Cape Horn, and the coast of Peru, is of much smaller size
than the P. gigantea, but, like it, of a dirty black colour. It
generally frequents the inland sounds in very large flocks:
I do not think I ever saw so many birds of any other sort
together, as I once saw of these behind the island of Chiloe.
Hundreds of thousands flew in an irregular line for several
hours in one direction. When part of the flock settled on the
308 CHARLES DARWIN
water the surface was blackened, and a noise proceeded from
them as of human beings talking in the distance.
There are several other species of petrels, but I will only
mention one other kind, the Pelacanoides Berardi, which
offers an example of those extraordinary cases, of a bird
evidently belonging to one well-marked family, yet both in
its habits and structure allied to a very distinct tribe. This
bird never leaves the quiet inland sounds. When disturbed
it dives to a distance, and on coming to the surface, with the
same movement takes flight. After flying by a rapid move-
ment of its short wings for a space in a straight line, it drops,
as if struck dead, and dives again. The form of its beak and
nostrils, length of foot, and even the colouring of its plum-
age, show that this bird is a petrel: on the other hand, its
short wings and consequent little power of flight, its form
of body and shape of tail, the absence of a hind toe to its
foot, its habit of diving, and its choice of situation, make it
at first doubtful whether its relationship is not equally close
with the auks. It would undoubtedly be mistaken for an auk,
when seen from a distance, either on the wing, or when div-
ing and quietly swimming about the retired channels of
Tierra del Fuego.
CHAPTER XIV
Chiloe and Concepcion : Great Earthquake
San Carlos, Chiloe — Osorno in eruption, contemporaneously with
Aconcagua and Coseguina — Ride to Cucao — Impenetrable Forests
— Valdivia Indians — Earthquake — Concepcion — Great Earthquake
— Rocks fissured — Appearance of the former Towns — The Sea Black
and Boiling — Direction of the Vibrations — Stones twisted round —
Great Wave — Permanent Elevation of the Land — Area of Volcanic
Phenomena — The connection between the Elevatory and Eruptive
Forces — Cause of Earthquakes — Slow Elevation of Mountain-
chains.
ON JANUARY the 15th we sailed from Low's Harbour,
and three days afterwards anchored a second time in
the bay of S. Carlos in Chiloe. On the night of the
jgth the volcano of Osorno was in action. At midnight the
sentry observed something like a large star, which gradually
increased in size till about three o'clock, when it presented
a very magnificent spectacle. By the aid of a glass, dark
objects, in constant succession, were seen, in the midst of a
great glare of red light, to be thrown up and to fall down.
The light was sufficient to cast on the water a long bright
reflection. Large masses of molten matter seem very com-
monly to be cast out of the craters in this part of the Cordil-
lera. I was assured that when the Corcovado is in eruption,
great masses are projected upwards and are seen to burst In
the air, assuming many fantastical forms, such as trees :
their size must be immense, for they can be distinguished
from the high land behind S. Carlos, which is no less than
ninety-three miles from the Corcovado. In the morning the
volcano became tranquil.
I was surprised at hearing afterwards that Aconcagua in
Chile, 480 miles northwards, was in action on the same night ;
and still more surprised to hear that the great eruption of
Coseguina (2700 miles north of Aconcagua), accompanied by
an earthquake felt over a 1000 miles, also occurred within
309
310 CHARLES DARWIN
six hours of this same time. This coincidence is the more
remarkable, as Coseguina had been dormant for twenty-six
years ; and Aconcagua most rarely shows any signs of action.
It is difficult even to conjecture whether this coincidence was
accidental, or shows some subterranean connection. If Vesu-
vius, Etna, and Hecla in Iceland (all three relatively nearer
each other than the corresponding points in South America),
suddenly burst forth in eruption on the same night, the coin-
cidence would be thought remarkable; but it is far more re-
markable in this case, where the three vents fall on the same
great mountain-chain, and where the vast plains along the
entire eastern coast, and the upraised recent shells along
more than 2000 miles on the western coast, show in how
equable and connected a manner the elevatory forces have
acted.
Captain Fitz Roy being anxious that some bearings should
be taken on the outer coast of Chiloe, it was planned that
Mr. King and myself should ride to Castro, and thence across
the island to the Capella de Cucao, situated on the west
coast. Having hired horses and a guide, we set out on
the morning of the 22nd. We had not proceeded far, before
we were joined by a woman and two boys, who were bent on
the same journey. Every one on this road acts on a " hail
fellow well met" fashion; and one may here enjoy the privi-
lege, so rare in South America, of travelling without fire-
arms. At first, the country consisted of a succession of hills
and valleys : nearer to Castro it became very level. The road
itself is a curious affair ; it consists in its whole length, with
the exception of very few parts, of great logs of wood, which
are either broad and laid longitudinally, or narrow and placed
transversely. In summer the road is not very bad; but in
winter, when the wood is rendered slippery from rain, trav-
elling is exceedingly difficult. At that time of the year, the
ground on each side becomes a morass, and is often over-
flowed: hence it is necessary that the longitudinal logs
should be fastened down by tranverse poles, which are
pegged on each side into the earth. These pegs render a fall
from a horse dangerous, as the chance of alighting on one of
them is not small. It is remarkable, however, how active
custom has made the Chilotan horses. In crossing bad parts,
THE VOYAGE OF THE BEAGLE 311
where the logs had been displaced, they skipped from one
to the other, almost with the quickness and certainty of a
dog. On both hands the road is bordered by the lofty forest-
trees, with their bases matted together by canes. When oc-
casionally a long reach of this avenue could be beheld, it pre-
sented a curious scene of uniformity: the white line of logs,
narrowing in perspective, became hidden by the gloomy forest,
or terminated in a zigzag which ascended some steep hill.
Although the distance from S. Carlos to Castro is only
twelve leagues in a straight line, the formation of the road
must have been a great labour. I was told that several peo-
ple had formerly lost their lives in attempting to cross the
forest. The first who succeeded was an Indian, who cut his
way through the canes in eight days, and reached S. Carlos :
he was rewarded by the Spanish government with a grant of
land. During the summer, many of the Indians wander
about the forests (but chiefly in the higher parts, where the
woods are not quite so thick) in search of the half-wild cattle
which live on the leaves of the cane and certain trees. It
was one of these huntsmen who by chance discovered, a few
years since, an English vessel, which had been wrecked on the
outer coast. The crew were beginning to fail in provisions,
and it is not probable that, without the aid of this man, they
would ever have extricated themselves from these scarcely
penetrable woods. As it was, one seaman died on the march,
from fatigue. The Indians in these excursions steer by the
sun ; so that if there is a continuance of cloudy weather, they
cannot travel.
The day was beautiful, and the number of trees which
were in full flower perfumed the air; yet even this could
hardly dissipate the effects of the gloomy dampness of the
forest. Moreover, the many dead trunks that stand like
skeletons, never fail to give to these primeval woods a char-
acter of solemnity, absent in those of countries long civilized.
Shortly after sunset we bivouacked for the night. Our fe-
male companion, who was rather good-looking, belonged to
one of the most respectable families in Castro: she rode,
however, astride, and without shoes or stockings. I was sur-
prised at the total want of pride shown by her and her brother.
They brought food with them, but at all our meals sat
312 CHARLES DARWIN
watching Mr. King and myself* whilst eating, till we were
fairly shamed into feeding the whole party. The night was
cloudless; and while lying in our beds, we enjoyed the sight
(and it is a high enjoyment) of the multitude of stars which
illumined the darkness of the forest.
January 23rd. — We rose early in the morning, and reached
the pretty quiet town of Castro by two o'clock. The old gov-
ernor had died since our last visit, and a Chileno was acting
in his place. We had a letter of introduction to Don Pedro,
whom we found exceedingly hospitable and kind, and more
disinterested than is usual on this side of the continent. The
next day Don Pedro procured us fresh horses, and offered
to accompany us himself. We proceeded to the south — gen-
erally following the coast, and passing through several ham-
lets, each with it's large barn-like chapel built of wood. At
Vilipilli, Don Pedro asked the commandant to give us a guide
to Cucao. The old gentleman offered to come himself; but
for a long time nothing would persuade him that two En-
glishmen really wished to go to such an out-of-the-way place
as Cucao. We were thus accompanied by the two greatest
aristocrats in the country, as was plainly to be seen in the
manner of all the poorer Indians towards them. At Chonchi
we struck across the island, following intricate winding
paths, sometimes passing through magnificent forests, and
sometimes through pretty cleared spots, abounding with corn
and potato crops. This undulating woody country, partially
cultivated, reminded me of the wilder parts of England, and
therefore had to my eye a most fascinating aspect. At Vi-
linco, which is situated on the borders of the lake of Cucao,
only a few fields were cleared; and all the inhabitants ap-
peared to be Indians. This lake is twelve miles long, and
runs in an east and west direction. From local circum-
stances, the sea-breeze blows very regularly during the day,
and during the night it falls calm : this has given rise to
strange exaggerations, for the phenomenon, as described to
us at S. Carlos, was quite a prodigy.
The road to Cucao was so very bad that we determined to
embark in a periagua. The commandant, in the most au-
thoritative manner, ordered six Indians to get ready to pull
us over, without deigning to tell them whether they would
THE VOYAGE OF THE BEAGLE 313
be paid. The periagua is a strange rough boat, but the crew
were still stranger: I doubt if six uglier little men ever got
into a boat together. They pulled, however, very well and
cheerfully. The stroke-oarsman gabbled Indian, and uttered
strange cries, much after the fashion of a pig-driver driving
his pigs. We started with a light breeze against us, but yet
reached the Capella de Cucao before it was late. The coun-
try on each side of the lake was one unbroken forest. In the
same periagua with us, a cow was embarked. To get so
large an animal into a small boat appears at first a difficulty,
but the Indians managed it in a minute. They brought the
cow alongside the boat, which was heeled towards her ; then
placing two oars under her belly, with their ends resting on
the gunwale, by the aid of these levers they fairly tumbled
the poor beast heels over head into the bottom of the boat,
and then lashed her down with ropes. At Cucao we found
an uninhabited hovel (which is the residence of the padre
when he pays this Capella a visit), where, lighting a fire, we
cooked our supper, and were very comfortable.
The district of Cucao is the only inhabited part on the
whole west coast of Chiloe. It contains about thirty or forty
Indian families, who are scattered along four or five miles
of the shore. They are very much secluded from the rest of
Chiloe, and have scarcely any sort of commerce, except
sometimes in a little oil, which they get from seal-blubber.
They are tolerably dressed in clothes of their own manu-
facture, and they have plenty to eat. They seemed, however,
discontented, yet humble to a degree which it was quite pain-
ful to witness. These feelings are, I think, chiefly to be
attributed to the harsh and authoritative manner in which
they are treated by their rulers. Our companions, although
so very civil to us, behaved to the poor Indians as if they
had been slaves, rather than free men. They ordered pro-
visions and the use of their horses, without ever condescend-
ing to say how much, or indeed whether the owners should
be paid at all. In the morning, being left alone with these
poor people, we soon ingratiated ourselves by presents of
cigars and mate. A lump of white sugar was divided be-
tween all present, and tasted with the greatest curiosity. The
Indians ended all their complaints by saying, "And it is only
314 CHARLES DARWIN
because we are poor Indians, and know nothing; but it was
not so when we had a King/'
The next day after breakfast, we rode a few miles north-
ward to Punta Huantamo. The road lay along a very broad
beach, on which, even after so many fine days, a terrible surf
was breaking. I was assured that after a heavy gale, the
roar can be heard at night even at Castro, a distance of no
less than twenty-one sea-miles across a hilly and wooded
country. We had some difficulty in reaching the point, owing
to the intolerably bad paths; for everywhere in the shade
the ground soon becomes a perfect quagmire. The point
itself is a bold rocky hill. It is covered by a plant allied, I
believe, to Bromelia, and called by the inhabitants Chepones.
In scrambling through the beds, our hands were very much
scratched. I was amused by observing the precaution our
Indian guide took, in turning up his trousers, thinking that
they were more delicate than his own hard skin. This plant
bears a fruit, in shape like an artichoke, in which a number
of seed-vessels are packed: these contain a pleasant sweet
pulp, here much esteemed. I saw at Low's Harbour the
Chilotans making chichi, or cider, with this fruit: so true is
it, as Humboldt remarks, that almost everywhere man finds
means of preparing some kind of beverage from the vege-
table kingdom. The savages, however, of Tierra del Fuego,
and I believe of Australia, have not advanced thus far in
the arts.
The coast to the north of Punta Huantamo is exceedingly
rugged and broken, and is fronted by many breakers, on
which the sea is eternally roaring. Mr. King and myself
were anxious to return, if it had been possible, on foot along
this coast; but even the Indians said it was quite imprac-
ticable. We were told that men have crossed by striking
directly through the woods from Cucao to S. Carlos, but
never by the coast. On these expeditions, the Indians carry
with them only roasted corn, and of this they eat sparingly
twice a day.
26th. — Re-embarking in the periagua, we returned across
the lake, and then mounted our horses. The whole of Chiloe
took advantage of this week of unusually fine weather, to
clear the ground by burning. In every direction volumes of
THE VOYAGE OF THE BEAGLE 315
smoke were curling upwards. Although the inhabitants were
so assiduous in setting fire to every part of the wood, yet
I did not see a single fire which they had succeeded in mak-
ing extensive. We dined with our friend the commandant,
and did not reach Castro till after dark. The next morning
we started very early. After having ridden for some time,
we obtained from the brow of a steep hill an extensive view
(and it is a rare thing on this road) of the great forest.
Over the horizon of trees, the volcano of Corcovado, and
the great flat-topped one to the north, stood out in proud
pre-eminence: scarcely another peak in the long range
showed its snowy summit. I hope it will be long before I
forget this farewell view of the magnificent Cordillera front-
ing Chiloe. At night we bivouacked under a cloudless sky,
and the next morning reached S. Carlos. We arrived on the
right day, for before evening heavy rain commenced.
February 4th. — Sailed from Chiloe. During the last week
I made several short excursions. One was to examine a
great bed of now-existing shells, elevated 350 feet above
the level of the sea: from among these shells, large forest-
trees were growing. Another ride was to P. Huechucucuy.
I had with me a guide who knew the country far too well;
for he would pertinaciously tell me endless Indian names for
every little point, rivulet, and creek. In the same manner as
in Tierra del Fuego, the Indian language appears singularly
well adapted for attaching names to the most trivial fea-
tures of the land. I believe every one was glad to say fare-
well to Chiloe; yet if we could forget the gloom and cease-
less rain of winter, Chiloe might pass for a charming island.
There is also something very attractive in the simplicity and
humble politeness of the poor inhabitants.
We steered northward along shore, but owing to thick
weather did not reach Valdivia till the night of the 8th. The
next morning the boat proceeded to the town, which is dis-
tant about ten miles. We followed the course of the river,
occasionally passing a few hovels, and patches of ground
cleared out of the otherwise unbroken forest; and sometimes
meeting a canoe with an Indian family. The town is situ-
ated on the low banks of the stream, and is so completely
buried in a wood of apple-trees that the streets are merely
316 CHARLES DARWIN
paths in an orchard. I have never seen any country, where
apple-trees appeared to thrive so well as in this damp part of
South America: on the borders of the roads there were
many young trees evidently self-grown. In Chiloe the in-
habitants possess a marvellously short method of making an
orchard. At the lower part of almost every branch, small,
conical, brown, wrinkled points project: these are always
ready to change into roots, as may sometimes be seen, where
any mud has been accidentally splashed against the tree. A
branch as thick as a man's thigh is chosen in the early spring,
and is cut off just beneath a group of these points, all the
smaller branches are lopped off, and it is then placed about
two feet deep in the ground. During the ensuing summer
the stump throws out long shoots, and sometimes even bears
fruit: I was shown one which had produced as many as
twenty-three apples, but this was thought very unusual. In
the third season the stump is changed (as I have myself
seen) into a well-wooded tree, loaded with fruit. An old
man near Valdivia illustrated his motto, u Necesidad es la
madre del invencion," by giving an account of the several
useful things he manufactured from his apples. After mak-
ing cider, and likewise wine, he extracted from the refuse a
white and finely flavoured spirit; by another process he pro-
cured a sweet treacle, or, as he called it, honey. His children
and pigs seemed almost to live, during this season of the
year, in his orchard.
February nth. — I set out with a guide on a short ride, in
which, however, I managed to see singularly little, either
of the geology of the country or of its inhabitants. There
is not much cleared land near Valdivia: after crossing a
river at the distance of a few miles, we entered the forest, and
then passed only one miserable hovel, before reaching our
sleeping-place for the night. The short difference in lati-
tude, of 150 miles, has given a new aspect to the forest, com-
pared with that of Chiloe. This is owing to a slightly
different proportion in the kinds of trees. The evergreens
do not appear to be quite so numerous, and the forest in
consequence has a brighter tint. As in Chiloe, the lower
parts are matted together by canes: here also another kind
(resembling the bamboo of Brazil and about twenty feet in
THE VOYAGE OF THE BEAGLE 317
height) grows in clusters, and ornaments the banks of some
of the streams in a very' pretty manner. It is with this plant
that the Indians make their chuzos, or long tapering spears.
Our resting-house was so dirty that I preferred sleeping out-
side: on these journeys the first night is generally very un-
comfortable, because one is not accustomed to the tickling
and biting of the fleas. I am sure, in the morning, there
was not a space on my legs the size of a shilling which had
not its little red mark where the flea had feasted.
1 2th. — We continued to ride through the uncleared forest ;
only occasionally meeting an Indian on horseback, or a troop
of fine mules bringing alerce-planks and corn from the south-
ern plains. In the afternoon one of the horses knocked up:
we were then on a brow of a hill, which commanded a fine
view of the Llanos. The view of these open plains was very
refreshing, after being hemmed in and buried in the wilder-
ness of trees. The uniformity of a forest soon becomes very
wearisome. This west coast makes me remember with pleas-
ure the free, unbounded plains of Patagonia; yet, with the
true spirit of contradiction, I cannot forget how sublime is
the silence of the forest. The Llanos are the most fertile
and thickly peopled parts of the country, as they possess the
immense advantage of being nearly free from trees. Before
leaving the forest we crossed some flat little lawns, around
which single trees stood, as in an English park: I have often
noticed with surprise, in wooded undulatory districts, that
the quite level parts have been destitute of trees. On ac-
count of the tired horse, I determined to stop at the Mission
of Cudico, to the friar of which I had a letter of introduc-
tion. Cudico is an intermediate district between the forest
and the Llanos. There are a good many cottages, with
patches of corn and potatoes, nearly all belonging to Indians.
The tribes dependent on Valdivia are " reducidos y cris-
tianos." The Indians farther northward, about Arauco and
Imperial, are still very wild, and not converted; but they
have all much intercourse with the Spaniards. The padre
said that the Christian Indians did not much like coming
to mass, but that otherwise they showed respect for religion.
The greatest difficulty is in making them observe the cere-
monies of marriage. The wild Indians take as many wives
318 CHARLES DARWIN
as they can support, and a cacique will sometimes have more
than ten : on entering his house, the number may be told by
that of the separate fires. Each wife lives a week in turn
with the cacique; but all are employed in weaving ponchos,
etc., for his profit. To be the wife of a cacique, is an honour
much sought after by the Indian women.
The men of all these tribes wear a coarse woolen poncho:
those south of Valdivia wear short trousers, and those north
of it a petticoat, like the chilipa of the Gauchos. All have
their long hair bound by a scarlet fillet, but with no other
covering on their heads. These Indians are good-sized men ;
their cheek-bones are prominent, and in general appearance
they resemble the great American family to which they be-
long; but their physiognomy seemed to me to be slightly
different from that of any other tribe which I had before
seen. Their expression is generally grave, and even austere,
and possesses much character : this may pass either for hon-
est bluntness or fierce determination. The long black hair,
the grave and much-lined features, and the dark complexion,
called to my mind old portraits of James I. On the road we
met with none of that humble politeness so universal in
Chiloe. Some gave their " mari-mari " (good morning) with
promptness, but the greater number did not seem inclined to
offer any salute. This independence of manners is probably
a consequence of their long wars, and the repeated victories
which they alone, of all the tribes in America, have gained
over the Spaniards.
I spent the evening very pleasantly, talking with the
padre. He was exceedingly kind and hospitable ; and coming
from Santiago, had contrived to surround himself with some
few comforts. Being a man of some little education, he bit-
terly complained of the total want of society. With no par-
ticular zeal for religion, no business or pursuit, how com-
pletely must this man's life be wasted ! The next day, on
our return, we met seven very wild-looking Indians, of whom
some were caciques that had just received from the Chilian
government their yearly small stipend for having long re-
mained faithful. They were fine-looking men, and they rode
one after the other, with most gloomy faces. An old cacique,
who headed them, had been, I suppose, more excessively
THE VOYAGE OF THE BEAGLE 319
drunk than the rest, for he seemed extremely grave and
very crabbed. Shortly before this, two Indians joined us,
who were travelling from a distant mission to Valdivia con-
cerning some lawsuit. One was a good-humoured old man,
but from his wrinkled beardless face looked more like an
old woman than a man. I frequently presented both of them
with cigars; and though ready to receive them, and I dare
say grateful, they would hardly condescend to thank me. A
Chilotan Indian would have taken off his hat, and given his
" Dios le page ! " The travelling was very tedious, both
from the badness of the roads, and from the number of great
fallen trees, which it was necessary either to leap over or to
avoid by making long circuits. We slept on the road, and
next morning reached Valdivia, whence I proceeded on
board.
A few days afterwards I crossed the bay with a party of
officers, and landed near the fort called Niebla. The build-
ings were in a most ruinous state, and the gun-carriages
quite rotten. Mr. Wickham remarked to the commanding
officer, that with one discharge they would certainly all fall
to pieces. The poor man, trying to put a good face upon it,
gravely replied, " No, I am sure, sir, they would stand
two ! " The Spaniards must have intended to have made this
place impregnable. There is now lying in the middle of the
court-yard a little mountain of mortar, which rivals in hard-
ness the rock on which it is placed. It was brought from
Chile, and cost 7000 dollars. The revolution having broken
out, prevented its being applied to any purpose, and now it
remains a monument of the fallen greatness of Spain.
I wanted to go to a house about a mile and a half distant,
but my guide said it was quite impossible to penetrate the
wood in a straight line. He offered, however, to lead me, by
following obscure cattle-tracks, the shortest way: the walk,
nevertheless, took no less than three hours ! This man is
employed in hunting strayed cattle; yet, well as he must
know the woods, he was not long since lost for two whole
days, and had nothing to eat. These facts convey a good
idea of the impracticability of the forests of these countries.
A question often occurred to me — how long does any vestige
of a fallen tree remain? This man showed me one which
320 CHARLES DARWIN
a party of fugitive royalists had cut down fourteen years
ago; and taking this as a criterion, I should think a bole a
foot and a half in diameter would in thirty years be changed
into a heap of mould.
February 20th. — This day has been memorable in the
annals of Valdivia, for the most severe earthquake experi-
enced by the oldest inhabitant. I happened to be on shore,
and was lying down in the wood to rest myself. It came on
suddenly, and lasted two minutes, but the time appeared
much longer. The rocking of the ground was very sensible.
The undulations appeared to my companion and myself to
come from due east, whilst others thought they proceeded
from south-west: this shows how difficult it sometimes is to
perceive the directions of the vibrations. There was no diffi-
culty in standing upright, but the motion made me almost
giddy: it was something like the movement of a vessel in a
little cross-ripple, or still more like that felt by a person skat-
ing over thin ice, which bends under the weight of his body.
A bad earthquake at once destroys our oldest associations :
the earth, the very emblem of solidity, has moved beneath
our feet like a thin crust over a fluid; — one second of time
has created in the mind a strange idea of insecurity, which
hours of reflection would not have produced. In the forest,
as a breeze moved the trees, I felt only the earth tremble, but
saw no other effect. Captain Fitz Roy and some officers
were at the town during the shock, and there the scene was
more striking; for although the houses, from being built of
wood, did not fall, they were violently shaken, and the boards
creaked and rattled together. The people rushed out of
doors in the greatest alarm. It is these accompaniments that
create that perfect horror of earthquakes, experienced by all
who have thus seen, as well as felt, their effects. Within the
forest it was a deeply interesting, but by no means an awe-
exciting phenomenon. The tides were very curiously affected.
The great shock took place at the time of low water;
and an old woman who was on the beach told me that the
water flowed very quickly, but not in great waves, to high-
water mark, and then as quickly returned to its proper level ;
this was also evident by the line of wet sand. The same kind
of quick but quiet movement in the tide happened a few
THE VOYAGE OF THE BEAGLE 321
years since at Chiloe, during a slight earthquake, and created
much causeless alarm. In the course of the evening there
were many weaker shocks, which seemed to produce in the
harbour the most complicated currents, and some of great
strength.
March 4th. — We entered the harbour of Concepcion. While
the ship was beating up to the anchorage, I landed on the
island of Quiriquina. The mayor-domo of the estate quickly
rode down to tell me the terrible news of the great earth-
quake of the 20th : — " That not a house in Concepcion or
Talcahuano (the port) was standing; that seventy villages
were destroyed; and that a great wave had almost washed
away the ruins of Talcahuano." Of this latter statement I
soon saw abundant proofs — the whole coast being strewed
over with timber and furniture as if a thousand ships had
been wrecked. Besides chairs, tables, book-shelves, etc., in
great numbers, there were several roofs of cottages, which
had been transported almost whole. The storehouses at Tal-
cahuano had been burst open, and great bags of cotton, yerba,
and other valuable merchandise were scattered on the shore.
During my walk round the island, I observed that numerous
fragments of rock, which, from the marine productions ad-
hering to them, must recently have been lying in deep water,
had been cast up high on the beach ; one of these was six feet
long, three broad, and two thick.
The island itself as plainly showed the overwhelming
power of the earthquake, as the beach did that of the conse-
quent great wave. The ground in many parts was fissured
in north and south lines, perhaps caused by the yielding of
the parallel and steep sides of this narrow island. Some of
the fissures near the cliffs were a yard wide. Many enormous
masses had already fallen on the beach; and the inhabitants
thought that when the rains commenced far greater slips would
happen. The effect of the vibration on the hard primary slate,
which composes the foundation of the island, was still more
curious: the superficial parts of some narrow ridges were as
completely shivered as if they had been blasted by gun-
powder. This effect, which was rendered conspicuous by the
fresh fractures and displaced soil, must be confined to near
vol. xxix — K HC
322 CHARLES DARWIN
the surface, for otherwise there would not exist a block of
solid rock throughout Chile; nor is this improbable, as it is
known that the surface of a vibrating body is affected differ-
ently from the central part. It is, perhaps, owing to this
same reason, that earthquakes do not cause quite such terrific
havoc within deep mines as would be expected. I believe this
convulsion has been more effectual in lessening the size of
the island of Quiriquina, than the ordinary wear-and-tear
of the sea and weather during the course of a whole century.
The next day I landed at Talcahuano, and afterwards rode
to Concepcion. Both towns presented the most awful yet
interesting spectacle I ever beheld. To a person who had
formerly know them, it possibly might have been still more
impressive ; for the ruins were so mingled together, and the
whole scene possessed so little the air of a habitable place,
that it was scarcely possible to imagine its former condition.
The earthquake commenced at half-past eleven o'clock in the
forenoon. If it had happened in the middle of the night, the
greater number of the inhabitants (which in this one prov-
ince must amount to many thousands) must have perished,
instead of less than a hundred : as it was, the invariable prac-
tice of running out of doors at the first trembling of the
ground, alone saved them. In Concepcion each house, or
row of houses, stood by itself, a heap or line of ruins ; but in
Talcahuano, owing to the great wave, little more than one
layer of bricks, tiles, and timber, with here and there part of
a wall left standing, could be distinguished. From this circum-
stance Concepcion, although not so completely desolated, was
a more terrible, and if I may so call it, picturesque sight.
The first shock was very sudden. The mayor-domo at Quiri-
quina told me, that the first notice he received of it, was
finding both the horse he rode and himself, rolling together
on the ground. Rising up, he was again thrown down. He
also told me that some cows which were standing on the steep
side of the island were rolled into the sea. The great wave
caused the destruction of many cattle; on one low island,
near the head of the bay, seventy animals were washed off
and drowned. It is generally thought that this has been the
worst earthquake ever recorded in Chile; but as the very
severe ones occur only after long intervals, this cannot easily
THE VOYAGE OF THE BEAGLE 323
be known ; nor indeed would a much worse shock have made
any difference, for the ruin was now complete. Innumerable
small tremblings followed the great earthquake, and within
the first twelve days no less than three hundred were counted.
After viewing Concepcion, I cannot understand how the
greater number of inhabitants escaped unhurt. The houses
in many parts fell outwards; thus forming in the middle of
the streets little hillocks of brickwork and rubbish. Mr.
Rouse, the English consul, told us that he was at breakfast
when the first movement warned him to run out. He had
scarcely reached the middle of the court-yard, when one side
of his house came thundering down. He retained presence
of mind to remember, that if he once got on the top of that
part which had already fallen, he would be safe. Not being
able from the motion of the ground to stand, he crawled up
on his hands and knees ; and no sooner had he ascended this
little eminence, than the other side of the house fell in, the
great beams sweeping close in front of his head. ■ With his
eyes blinded, and his mouth choked with the cloud of dust
which darkened the sky, at last he gained the street. As
shock succeeded shock, at the interval of a few minutes, no
one dared approach the shattered ruins; and no one knew
whether his dearest friends and relations were not perish-
ing from the want of help. Those who had saved any prop-
erty were obliged to keep a constant watch, for thieves
prowled about, and at each little trembling of the ground,
with one hand they beat their breasts and cried " Miseri-
cordia ! " and then with the other filched what they could
from the ruins. The thatched roofs fell over the fires, and
flames burst forth in all parts. Hundreds knew themselves
ruined, and few had the means of providing food for the day.
Earthquakes alone are sufficient to destroy the prosperity
of any country. If beneath England the now inert subter-
ranean forces should exert those powers, which most assur-
edly in former geological ages they have exerted, how com-
pletely would the entire condition of the country be changed !
What would become of the lofty houses, thickly packed cities,
great manufactories, the beautiful public and private edi-
fices? If the new period of disturbance were first to com-
mence by some great earthquake in the dead of the night,
324 CHARLES DARWIN
how terrific would be the carnage ! England would at once
be bankrupt; all papers, records, and accounts would from
that moment be lost. Government being unable to collect
the taxes, and failing to maintain its authority, the hand of
violence and rapine would remain uncontrolled. In every
large town famine would go forth, pestilence and death fol-
lowing in its train.
Shortly after the shock, a great wave was seen from the
distance of three or four miles, approaching in the middie
of the bay with a smooth outline; but along the shore it tore
up cottages and trees, as it swept onwards with irresistible
force. At the head of the bay it broke in a fearful line of
white breakers, which rushed up to a height of 23 vertical
feet above the highest spring-tides. Their force must have
been prodigious ; for at the Fort a cannon with its carriage,
estimated at four tons in weight, was moved 15 feet inwards.
A schooner was left in the midst of the ruins, 200 yards
from the beach. The first wave was followed by two others,
which in their retreat carried away a vast wreck of floating
objects. In one part of the bay, a ship was pitched high
and dry on shore, was carried off, again driven on shore, and
again carried off. In another part, two large vessels anchored
near together were whirled about, and their cables were thrice
wound round each other; though anchored at a depth of 36
feet, they were for some minutes aground. The great wave-
must have travelled slowly, for the inhabitants of Talca-
huano had time to run up the hills behind the town; and
some sailors pulled out seaward, trusting successfully to their
boat riding securely over the swell, if they could reach it
before it broke. One old woman with a little boy, four or
five years old, ran into a boat, but there was nobody to row
it out: the boat was consequently dashed against an anchor
and cut in twain ; the old woman was drowned, but the child
was picked up some hours afterwards clinging to the wreck.
Pools of salt-water were still standing amidst the ruins of
the houses, and children, making boats with old tables and
chairs, appeared as happy as their parents were miserable.
It was, however, exceedingly interesting to observe, how
much more active and cheerful all appeared than could have
been expected. It was remarked with much truth, that from
THE VOYAGE OF THE BEAGLE 325
the destruction being universal, no one individual was hum-
bled more than another, or could suspect his friends of cold-
ness — that most grievous result of the loss of wealth. Mr.
Rouse, and a large party whom he kindly took under his
protection, lived for the first week in a garden beneath some
apple-trees. At first they were as merry as if it had been a
picnic ; but soon afterwards heavy rain caused much discom-
fort, for they were absolutely without shelter.
In Captain Fitz Roy's excellent account of the earthquake,
it is said that two explosions, one like a column of smoke and
another like the blowing of a great whale, were seen in the
bay. The water also appeared everywhere to be boiling ; and
it " became black, and exhaled a most disagreeable sulphure-
ous smell." These latter circumstances were observed in the
Bay of Valparaiso during the earthquake of 1822 ; they may,
I think, be accounted for, by the disturbance of the mud at
the bottom of the sea containing organic matter in decay. In
the Bay of Callao, during a calm day, I noticed, that as the
ship dragged her cable over the bottom, its course was marked
by a line of bubbles. The lower orders in Talcahuano thought
that the earthquake was caused by some old Indian women, ■
who two years ago, being offended, stopped the volcano of
Antuco. This silly belief is curious, because it shows that
experience has taught them to observe, that there exists a
relation between the suppressed action of the volcanos, and
the trembling of the ground. It was necessary to apply the
witchcraft to the point where their perception of cause and
effect failed; and this was the closing of the volcanic vent.
This belief is the more singular in this particular instance,
because, according to Captain Fitz Roy, there is reason to
believe that Antuco was noways affected.
The town of Concepcion was built in the usual Spanish
fashion, with all the streets running at right angles to each
other; one set ranging S.W. by W., and the other set N.W.
by N. The walls in the former direction certainly stood
better than those in the latter; the greater number of the
masses of brickwork were thrown down towards the N.E.
Both these circumstances perfectly agree with the general
idea, of the undulations having come from the S.W., in which
quarter subterranean noises were also heard ; for it is evident
326 CHARLES DARWIN
that the walls running S.W. and N.E. which presented their
ends to the point whence the undulations came, would be
much less likely to fall than those walls which, running N.W.
and S.E., must in their whole lengths have been at the same
instant thrown out of the perpendicular ; for the undulations,
coming from the S.W., must have extended in N.W. and
S.E. waves, as they passed under the foundations. This may
be illustrated by placing books edgeways on a carpet, and
then, after the manner suggested by Michell, imitating the
undulations of an earthquake : it will be found that they fall
with more or less readiness, according as their direction more
or less nearly coincides with the line of the waves. The fis-
sures in the ground generally, though not uniformly, extended
in a S.E. and N.W. direction, and therefore corresponded
to the lines of undulation or of principal flexure. Bearing in
mind all these circumstances, which so clearly point to the
S.W. as the chief focus of disturbance, it is a very interesting
fact that the island of S. Maria, situated in that quarter, was,
during the general uplifting of the land, raised to nearly
three times the height of any other part of the coast.
The different resistance offered by the walls, according to
their direction, was well exemplified in the case of the Cathe-
dral. The side which fronted the N.E. presented a grand
pile of ruins, in the midst of which door-cases and masses
of timber stood up, as if floating in a stream. Some of the
angular blocks of brickwork were of great dimensions; and
they were rolled to a distance on the level plaza, like frag-
ments of rock at the base of some high mountain. The side
walls (running S.W. and N.E.), though exceedingly frac-
tured, yet remained standing; but the vast buttresses (at
right angles to them, and therefore parallel to the walls that
fell) were in many cases cut clean off, as if by a chisel, and
hurled to the ground. Some square ornaments on the cop-
ing of these same walls, were moved by the earthquake into
a diagonal position. A similar circumstance was observed
after an earthquake at Valparaiso, Calabria, and other places,
including some of the ancient Greek temples. 1 This twist-
ing displacement, at first appears to indicate a vorticose
1 M. Arago in L'Institut, 1839, p. 337. See also Miers's Chile, vol. i. p.
392; also Lyell's Principles of Geology, chap, xv., book ii.
THE VOYAGE OF THE BEAGLE 327
movement beneath each point thus affected ; but this is highly
improbable. May it not be caused by a tendency in each stone
to arrange itself in some particular position, with respect
to the lines of vibration, — in a manner somewhat similar to
pins on a sheet of paper when shaken ? Generally speaking,
arched doorways or windows stood much better than any
other part of the buildings. Nevertheless, a poor lame old
man, who had been in the habit, during trifling shocks, of
crawling to a certain doorway, was this time crushed to
pieces.
I have not attempted to give any detailed description of
the appearance of Concepcion, for I feel that it is quite impos-
sible to convey the mingled feelings which I experienced.
Several of the officers visited it before me, but their strongest
language failed to give a just idea of the scene of desolation.
It is a bitter and humiliating thing to see works, which have
cost man so much time and labour, overthrown in one min-
ute; yet compassion for the inhabitants was almost instantly
banished, by the surprise in seeing a state of things produced
in a moment of time, which one was accustomed to attribute
to a succession of ages. In my opinion, we have scarcely be-
held, since leaving England, any sight so deeply interesting.
In almost every severe earthquake, the neighbouring waters
of the sea are said to have been greatly agitated. The dis-
turbance seems generally, as in the case of Concepcion, to
have been of two kinds: first, at the instant of the shock,
the water swells high up on the beach with a gentle motion,
and then as quietly retreats ; secondly, some time afterwards,
the whole body of the sea retires from the coast, and then
returns in waves of overwhelming force. The first move-
ment seems to be an immediate consequence of the earth-
quake affecting differently a fluid and a solid, so that their
respective levels are slightly deranged: but the second case
is a far more important phenomenon. During most earth-
quakes, and especially during those on the west coast of
America, it is certain that the first great movement of the
waters has been a retirement. Some authors have attempted
to explain this, by supposing that the water retains its level,
whilst the land oscillates upwards ; but surely the water close
to the land, even on a rather steep coast, would partake of the
328 CHARLES DARWIN
motion of the bottom : moreover, as urged by Mr. Lyell,
similar movements of the sea have occurred at islands far
distant from the chief line of disturbance, as was the case
with Juan Fernandez during this earthquake, and with
Madeira during the famous Lisbon shock. I suspect (but the
subject is a very obscure one) that a wave, however produced,
first draws the water from the shore, on which it is advancing
to break: I have observed that this happens with the little
waves from the paddles of a steam-boat. It is remarkable
that whilst Talcahuano and Callao (near Lima), both situ-
ated at the head of large shallow bays, have suffered during
every severe earthquake from great waves, Valparaiso,
seated close to the edge of profoundly deep water, has never
been overwhelmed, though so often shaken by the severest
shocks. From the great wave not immediately following the
earthquake, but sometimes after the interval of even half an
hour, and from distant islands being affected similarly with
the coasts near the focus of the disturbance, it appears that
the wave first rises in the offing; and as this is of general
occurrence, the cause must be general: I suspect we must
look to the line, where the less disturbed waters of the deep
ocean join the water nearer the coast, which has partaken
of the movements of the land, as the place where the great
wave is first generated; it would also appear that the wave
is larger or smaller, according to the extent of shoal water
which has been agitated together with the bottom on which it
rested.
The most remarkable effect of this earthquake was the per-
manent elevation of the land ; it would probably be far more
correct to speak of it as the cause. There can be no doubt
that the land round the Bay of Concepcion was upraised
two or three feet; but it deserves notice, that owing to the
wave having obliterated the old lines of tidal action on the
sloping sandy shores, I could discover no evidence of this
fact, except in the united testimony of the inhabitants, that
one little rocky shoal, now exposed, was formerly covered
with water. At the island of S. Maria (about thirty miles
distant) the elevation was greater; on one part, Captain Fitz
Roy founds beds of putrid mussel-shells still adhering to the
THE VOYAGE OF THE BEAGLE 329
rocks, ten feet above high-water mark: the inhabitants had
formerly dived at lower-water spring-tides for these shells.
The elevation of this province is particularly interesting,
from its having been the theatre of several other violent
earthquakes, and /from the vast numbers of sea-shells scat-
tered over the land, up to a height of certainly 600, and I
believe, of 1000 feet. At Valparaiso, as I have remarked,
similar shells are found at the height of 1300 feet: it is hardly
possible to doubt that this great elevation has been effected
by successive small uprisings, such as that which accompa-
nied or caused the earthquake of this year, and likewise by
an insensibly slow rise, which is certainly in progress on
some parts of this coast. \
The island of Juan Fernandez, 360 miles to the N.E., was,
at the time of the great shock of the 20th, violently shaken,
so that the trees beat against each other, and a volcano burst
forth under water close to the shore : these facts are remark-
able because this island, during the earthquake of 1751, was
then also affected more violently than other places at an equal
distance from Concepcion, and this seems to show some sub-
terranean connection between these two points. Chiloe, about
340 miles southward of Concepcion, appears to have been
shaken more strongly than the intermediate district of Val-
divia, where the volcano of Villarica was noways affected,
whilst in the Cordillera in front of Chiloe, two of the vol-
canos burst -forth at the same instant in violent action. These
two volcanos, and some neighbouring ones, continued for a
long time in eruption, and ten months afterwards were
again influenced by an earthquake at Concepcion. Some
men, cutting wood near the base of one of these volcanos,
did not perceive the shock of the 20th, although the whole
surrounding Province was then trembling; here we have an
eruption relieving and taking the place of an earthquake,
as would have happened at Concepcion, according to the
belief of the lower orders, if the volcano at Antuco had not
been closed by witchcraft. Two years and three-quarters
afterwards, Valdivia and Chiloe were again shaken, more
violently than on the 20th, and an island in the Chonos
Archipelago was permanently elevated more than eight feet.
It will give a better idea of the scale of these phenomena, if
330 CHARLES DARWIN
(as in the case of the glaciers) we suppose them to have
taken place at corresponding distances in Europe : — then
would the land from the North Sea to the Mediterranean
have been violently shaken, and at the same instant of time a
large tract of the eastern coast of England would have been
permanently elevated, together with some outlying islands, — a
train of volcanos on the coast of Holland would have burst
forth in action, and an eruption taken place at the bottom of
the sea, near the northern extremity of Ireland — and lastly,
the ancient vents of Auvergne, Cantal, and Mont d'Or would
each have sent up to the sky a dark column of smoke, and
have long remained in fierce action. Two years and three-
quarters afterwards, France, from its centre to the English
Channel, would have been again desolated by an earthquake,
and an island permanently upraised in the Mediterranean.
The space, from under which volcanic matter on the 20th
was actually erupted, is 720 miles in one line, and 400 miles
in another line at right angles to the first : hence, in all prob-
ability, a subterranean lake of lava is here stretched out, of
nearly double the area of the Black Sea. From the intimate
and complicated manner in which the elevatory and eruptive
forces were shown to be connected during this train of phe-
nomena, we may confidently come to the conclusion, that the
forces which slowly and by little starts uplift continents, and
those which at successive periods pour forth volcanic matter
from open orifices, are identical. From many reasons, I
believe that the frequent quakings of the earth on this line
of coast are caused by the rending of the strata, necessarily
consequent on the tension of the land when upraised, and
their injection by fluidified rock. This rending and injection
would, if repeated often enough (and we know that earth-
quakes repeatedly affect the same areas in the same manner),
form a chain of hills; — and the linear island of S. Mary,
which was upraised thrice the height of the neighbouring
country, seems to be undergoing this process. I believe that
the solid axis of a mountain, differs in its manner of forma-
tion from a volcanic hill, only in the molten stone having
been repeatedly injected, instead of having been repeatedly
ejected. Moreover, I believe that it is impossible to explain
the structure of great mountain-chains, such as that of the
THE VOYAGE OF THE BEAGLE 331
Cordillera, where the strata, capping the injected axis of
plutonic rock, have been thrown on their edges along several
parallel and neighbouring lines of elevation, except on this
view of the rock of the axis having been repeatedly injected,
after intervals sufficiently long to allow the upper parts or
wedges to cool and become solid; — for if the strata had been
thrown into their present highly inclined, vertical, and even
inverted positions, by a single blow, the very bowels of the
earth would have gushed out; and instead of beholding abrupt
mountain-axes of rock solidified under great pressure, deluges
of lava would have flowed out at innumerable points on every
line of elevation. 2
3 For a full account of the volcanic phenomena which accompanied the
earthquake of the 20th, and for the conclusions deducible from them, I must
refer to Volume V. of the Geological Transactions.
CHAPTER XV
Passage of the Cordillera
Valparaiso — Portillo Pass — Sagacity of Mules — Mountain-torrents —
Mines, how discovered — Proofs of the gradual Elevation of the
Cordillera — Effect of Snow on Rocks — Geological Structure of the
two main Ranges, their distinct Origin and Upheaval — Great Sub-
sidence — Red Snow — Winds — Pinnacles of Snow — Dry and clear
Atmosphere — Electricity — Pampas — Zoology of the opposite Side
of the Andes — Locusts — Great Bugs — Mendoza — Uspallata Pass —
Silicified Trees buried as they grew — Incas Bridge — Badness of
the Passes exaggerated — Cumbre — Casuchas — Valparaiso.
T\ /fr^RCH 7th> I $35' — We stayed three days at Concep-
Iwm c * on > an d then sailed for Valparaiso. The wind
being northerly, we only reached the mouth of the
harbour of Concepcion before it was dark. Being very near
the land, and a fog coming on, the anchor was dropped.
Presently a large American whaler appeared alongside of us ;
and we heard the Yankee swearing at his men to keep quiet,
whilst he listened for the breakers. Captain Fitz Roy hailed
him, in a loud clear voice, to anchor where he then was. The
poor man must have thought the voice came from the shore :
such a Babel of cries issued at once from the ship — every
one hallooing out, " Let go the anchor ! veer cable ! shorten
sail ! " It was the most laughable thing I ever heard. If
the ship's crew had been all captains, and no men, there could
not have been a greater uproar of orders. We afterwards
found that the mate stuttered: I suppose all hands were
assisting him in giving his orders.
On the nth we anchored at Valparaiso, and two days
afterwards I set out to cross the Cordillera. I proceeded to
Santiago, where Mr. Caldcleugh most kindly assisted me in
every possible way in making the little preparations which
were necessary. In this part of Chile there are two passes
across the Andes to Mendoza: the one most commonly used
— namely, that of Aconcagua or Uspallata — is situated some
332
THE VOYAGE OF THE BEAGLE 333
way to the north; the other, called the Portillo, is to the
south, and nearer, but more lofty and dangerous.
March 18th. — We set out for the Portillo pass. Leaving
Santiago we crossed the wide burnt-up plain on which that
city stands, and in the afternoon arrived at the Maypu, one
of the principal rivers in Chile. The valley, at the point
where it enters the first Cordillera, is bounded on each side
by lofty barren mountains; and although not broad, it is very
fertile. Numerous cottages were surrounded by vines, and by
orchards of apple, nectarine, and peach-trees — their boughs
breaking with the weight of the beautiful ripe fruit. In the
evening we passed the custom-house, where our luggage was
examined. The frontier of Chile is better guarded by the
Cordillera, than by the waters of the sea. There are very
few valleys which lead to the central ranges, and the
mountains are quite impassable in other parts by beasts of
burden. The custom-house officers were very civil, which
was perhaps partly owing to the passport which the President
of the Republic had given me; but I must express my admira-
tion at the natural politeness of almost every Chileno. In
this instance, the contrast with the same class of men in
most other countries was strongly marked. I may mention
an anecdote with which I was at the time much pleased : we
met near Mendoza a little and very fat negress, riding astride
on a mule. She had a goitre so enormous that it was scarcely
possible to avoid gazing at her for a moment; but my two
companions almost instantly, by way of apology, made the
common salute of the country by taking off their hats. Where
would one of the lower or higher classes in Europe, have
shown such feeling politeness to a poor and miserable object
of a degraded race?
At night we slept at a cottage. Our manner of travelling
was delightfully independent. In the inhabited parts we
bought a little firewood, hired pasture for the animals, and
bivouacked in the corner of the same field with them. Car-
rying an iron pot, we cooked and ate our supper under a
cloudless sky, and knew no trouble. My companions were
Mariano Gonzales, who had formerly accompanied me in
Chile, and an " arriero," with his ten mules and a " madrina."
The madrina (or godmother) is a most important personage:
334 CHARLES DARWIN
she is an old steady mare, with a little bell round her neck;
and wherever she goes, the mules, like good children, follow
her. The affection of these animals for their madrinas saves
infinite trouble. If several large troops are turned into one
field to graze, in the morning the muleteers have only to lead
the madrinas a little apart, and tinkle their bells; although
there may be two or three hundred together, each mule im-
mediately knows the bell of its own madrina, and comes to
her. It is nearly impossible to lose an old mule; for if
detained for several hours by force, she will, by the power
of smell, like a dog, track out her companions, or rather the
madrina, for, according to the muleteer, she is the chief
object of affection. The feeling, however, is not of an indi-
vidual nature; for I believe I am right in saying that any
animal with a bell will serve as a madrina. In a troop each
animal carries on a level road, a cargo weighing 416 pounds
(more than 29 stone), but in a mountainous country 100
pounds less; yet with what delicate slim limbs, without any
proportional bulk of muscle, these animals support so great
a burden ! The mule always appears to me a most surprising
animal. That a hybrid should possess more reason, memory,
obstinacy, social affection, powers of muscular endurance,
and length of life, than either of its parents, seems to indi-
cate that art has here outdone nature. Of our ten animals,
six were intended for riding, and four for carrying cargoes,
each taking turn about. We carried a good deal of food, in
case we should be snowed up, as the season was rather late
for passing the Portillo.
March ipth. — We rode during this day to the last, and
therefore most elevated, house in the valley. The number of
inhabitants became scanty; but wherever water could be
brought on the land, it was very fertile. All the main valleys
in the Cordillera are characterized by having, on both sides, a
fringe or terrace of shingle and sand, rudely stratified, and
generally of considerable thickness. These fringes evidently
once extended across the valleys and were united; and the
bottoms of the valleys in northern Chile, where there are no
streams, are thus smoothly filled up. On these fringes the
roads are generally carried, for their surfaces are even, and
they rise with a very gentle slope up the valleys : hence, also,
THE VOYAGE OF THE BEAGLE 335
they are easily cultivated by irrigation. They may be traced
up to a height of between 7000 and 9000 feet, where they
become hidden by the irregular piles of debris. At the lower
end or mouths of the valleys, they are continuously united to
those land-locked plains (also formed of shingle) at the foot
of the main Cordillera, which I have described in a former
chapter as characteristic of the scenery of Chile, and which
were undoubtedly deposited when the sea penetrated Chile, as
it now does the more southern coasts. No one fact in the
geology of South America, interested me more than these
terraces of rudely-stratified shingle. They precisely resemble
in composition the matter which the torrents in each valley
would deposit, if they were checked in their course by any
cause, such as entering a lake or arm of the sea; but the
torrents, instead of depositing matter, are now steadily at
work wearing away both the solid rock and these alluvial
deposits, along the whole line of every main valley and side
valley. It is impossible here to give the reasons, but I am
convinced that the shingle terraces were accumulated, during
the gradual elevation of the Cordillera, by the torrents
delivering, at successive levels, their detritus on the beach-
heads of long narrow arms of the sea, first high up the val-
leys, then lower and lower down as the land slowly rose. If
this be so, and I cannot doubt it, the grand and broken chain
of the Cordillera, instead of having been suddenly thrown up,
as was till lately the universal, and still is the common opinion
of geologists, has been slowly upheaved in mass, in the same
gradual manner as the coasts of the Atlantic and Pacific have
risen within the recent period. A multitude of facts in the
structure of the Cordillera, on this view receive a simple
explanation.
The rivers which flow in these valleys ought rather to be
called mountain-torrents. Their inclination is very great,
and their water the colour of mud. The roar which the
Maypu made, as it rushed over the great rounded fragments,
was like that of the sea. Amidst the din of rushing waters,
the noise from the stones, as they rattled one over another,
was most distinctly audible even from a distance. This rat-
tling noise, night and day, may be heard along the whole
course of the torrent. The sound spoke eloquently to the
336 CHARLES DARWIN
geologist; the thousands and thousands of stones, which,
striking against each other, made the one dull uniform sound,
were all hurrying in one direction. It was like thinking on
time, where the minute that now glides past is irrevocable.
So was it with these stones; the ocean is their eternity, and
each note of that wild music told of one more step towards
their destiny.
It is not possible for the mind to comprehend, except by
a slow process, any effect which is produced by a cause re-
peated so often, that the multiplier itself conveys an idea,
not more definite than the savage implies when he points to
the hairs of his head. As often as I have seen beds of mud,
sand, and shingle, accumulated to the thickness of many
thousand feet, I have felt incline j. to exclaim that causes,
such as the present rivers and the present beaches, could
never have ground down and produced such masses. But, on
the other hand, when listening to the rattling noise of these
torrents, and calling to mind that whole races of animals have
passed away from the face of the earth, and that during this
whole period, night and day, these stones have gone rattling
onwards in their course, I have thought to myself, can any
mountains, any continent, withstand such waste?
In this part of the valley, the mountains on each side were
from 3000 to 6000 or 8000 feet high, with rounded outlines
and steep bare flanks. The general colour of the rock was
dullish purple, and the stratification very distinct. If the
scenery was not beautiful, it was remarkable and grand. We
met during the day several herds of cattle, which men were
driving down from the higher valleys in the Cordillera. This
sign of the approaching winter hurried our steps, more than
was convenient for geologizing. The house where we slept
was situated at the foot of a mountain, on the summit of
which are the mines of S. Pedro de Nolasko. Sir F. Head
marvels how mines have been discovered in such extraordi-
nary situations, as the bleak summit of the mountain of S.
Pedro de Nolasko. In the first place, metallic veins in this
country are generally harder than the surrounding strata:
hence, during the gradual wear of the hills, they project
above the surface of the ground. Secondly, almost every
labourer, especially in the northern parts of Chile, under-
THE VOYAGE OF THE BEAGLE 337
stands something about the appearance of ores. In the great
mining provinces of Coquimbo and Copiapo, firewood is very
scarce, and men search for it over every hill and dale; and
by this means nearly all the richest mines have there been
discovered. Chanuncillo, from which silver to the value of
many hundred thousand pounds has been raised in the course
of a few years, was discovered by a man who threw a stone
at his loaded donkey, and thinking that it was very heavy, he
picked it up, and found it full of pure silver: the vein oc-
curred at no great distance, standing up like a wedge of
metal. The miners, also, taking a crowbar with them, often
wander on Sundays over the mountains. In this south part
of Chile, the men who drive cattle into the Cordillera, and
who frequent every ravine where there is a little pasture, are
the usual discoverers.
20th. — As we ascended the valley, the vegetation, with
the exception of a few pretty alpine flowers, became exceed-
ingly scanty; and of quadrupeds, birds, or insects, scarcely
one could be seen. The lofty mountains, their summits
marked with a few patches of snow, stood well separated
from each other, the valleys being filled up with an immense
thickness of stratified alluvium. The features in the scenery
of the Andes which struck me most, as contrasted with the
other mountain chains with which I am acquainted, were, —
the flat fringes sometimes expanding into narrow plains on
each side of the valleys, — the bright colours, chiefly red and
purple, of the utterly bare and precipitous hills of porphyry,
the grand and continuous wall-like dykes, — the plainly-
divided strata which, where nearly vertical, formed the pic-
turesque and wild central pinnacles, but where less inclined,
composed the great massive mountains on the outskirts of the
range, — and lastly, the smooth conical piles of fine and
brightly coloured detritus, which sloped up at a high angle
from the base of the mountains, sometimes to a height of
more than 2000 feet.
I frequently observed, both in Tierra del Fuego and within
the Andes, that where the rock was covered during the greater
part of the year with snow, it was shivered in a very extraor-
dinary manner into small angular fragments. Scoresby 1
1 Scoresby's Arctic Regions, vol. i. p. 122.
338 CHARLES DARWIN
has observed the same fact in Spitzbergen. The case
appears to me rather obscure: for that part of the mountain
which is protected by a mantle of snow, must be less subject
to repeated and great changes of temperature than any other
part. I have sometimes thought, that the earth and frag-
ments of stone on the surface, were perhaps less effectually
removed by slowly percolating snow-water 2 than by rain, and
therefore that the appearance of a quicker disintegration of
the solid rock under the snow, was deceptive. Whatever the
cause may be, the quantity of crumbling stone on the Cordil-
lera is very great. Occasionally in the spring, great masses
of this detritus slide down the mountains, and cover the
snow-drifts in the valleys, thus forming natural ice-houses.
We rode over one, the height of which was far below the
limit of perpetual snow.
As the evening drew to a close, we reached a singular
basin-like plain, called the Valle del Yeso. It was covered
by a little dry pasture, and we had the pleasant sight of a
herd of cattle amidst the surrounding rocky deserts. The
valley takes its name of Yeso from a great bed, I should think
at least 2000 feet thick, of white, and in some parts quite
pure, gypsum. We slept with a party of men, who were
employed in loading mules with this substance, which is used
in the manufacture of wine. We set out early in the morning
(21st), and continued to follow the course of the river, which
had become very small, till we arrived at the foot of the ridge,
that separates the waters flowing into the Pacific and Atlantic
Oceans. The road, which as yet had been good with a steady
but very gradual ascent, now changed into a steep zigzag
track up the great range, dividing the republics of Chile
and Mendoza.
I will here give a very brief sketch of the geology of the
several parallel lines forming the Cordillera. Of these lines,
there are two considerably higher than the others; namely,
on the Chilian side, the Peuquenes ridge, which, where the
road crosses it, is 13,210 feet above the sea; and the Portillo
3 I have heard it remarked in Shropshire that the water, when the Severn
is flooded from long-continued rain, is much more turbid than when it
proceeds from the snow melting in the Welsh mountains. D'Orbigny (torn.
1. p. 184), in explaining the cause of the various colours of the rivers in
South America, remarks that those with blue or clear water have their
source in the Cordillera, where the snow melts.
THE VOYAGE OF THE BEAGLE 339
ridge, on the Mendoza side, which is 14,305 feet. The lower
beds of the Peuquenes ridge, and of the several great lines
to the westward of it, are composed of a vast pile, many thou-
sand feet in thickness, of porphyries which have flowed as
submarine lavas, alternating with angular and rounded frag-
ments of the same rocks, thrown out of the submarine craters.
These alternating masses are covered in the central parts,
by a great thickness of red sandstone, conglomerate, and cal-
careous clay-slate, associated with, and passing into, pro-
digious beds of gypsum. In these upper beds shells are toler-
ably frequent; and they belong to about the period of the
lower chalk of Europe. It is an old story, but not the less
wonderful, to hear of shells which were once crawling on the
bottom of the sea, now standing nearly 14,000 feet above its
level. The lower beds in this great pile of strata, have been
dislocated, baked, crystallized and almost blended together,
through the agency of mountain masses of a peculiar white
soda-granitic rock.
The other main line, namely, that of the Portillo, is of a
totally different formation: it consists chiefly of grand bare
pinnacles of a red potash-granite, which low down on the
western flank are covered by a sandstone, converted by the
former heat into a quartz-rock. On the quartz, there rest
beds of a conglomerate several thousand feet in thickness,
which have been upheaved by the red granite, and dip at an
angle of 45 towards the Peuquenes line. I was astonished
to find that this conglomerate was partly composed of peb-
bles, derived from the rocks, with their fossil shells, of the
Peuquenes range; and partly of red potash-granite, like that
of the Portillo. Hence we must conclude, that both the Peu-
quenes and Portillo ranges were partially upheaved and ex-
posed to wear and tear, when the conglomerate was forming ;
but as the beds of the conglomerate have been thrown off at
an angle of 45 by the red Portillo granite (with the under-
lying sandstone baked by it), we may feel sure, that the
greater part of the injection and upheaval of the already
partially formed Portillo line, took place after the accumula-
tion of the conglomerate, and long after the elevation of the
Peuquenes ridge. So that the Portillo, the loftiest line in this
part of the Cordillera, is not so old as the less lofty line of
340 CHARLES DARWIN
the Peuquenes. Evidence derived from an inclined stream
of lava at the eastern base of the Portillo, might be adduced
to show, that it owes part of its great height to elevations of
a still later date. Looking to its earliest origin, the red gran-
ite seems to have been injected on an ancient pre-existing line
of white granite and mica-slate. In most parts, perhaps in
all parts, of the Cordillera, it may be concluded that each line
has been formed by repeated upheavals and injections; and
that the several parallel lines are of different ages. Only
thus can we gain time, at all sufficient to explain the truly
astonishing amount of denudation, which these great, though
comparatively with most other ranges recent, mountains have
suffered.
Finally, the shells in the Peuquenes or oldest ridge, prove,
as before remarked, that it has been upraised 14,000 feet
since a Secondary period, which in Europe we are accus-
tomed to consider as far from ancient; but since these shells
lived in a moderately deep sea, it can be shown that the area
now occupied by the Cordillera, must have subsided several
thousand feet — in northern Chile as much as 6000 feet — so
as to have allowed that amount of submarine strata to have
been heaped on the bed on which the shells lived. The proof
is the same with that by which it was shown, that at a much
later period, since the tertiary shells of Patagonia lived,
there must have been there a subsidence of several hundred
feet, as well as an ensuing elevation. Daily it is forced home
on the mind of the geologist, that nothing, not even the wind
that blows, is so unstable as the level of the crust of this
earth.
I will make only one other geological remark : although
the Portillo chain is here higher than the Peuquenes, the
waters draining the intermediate valleys, have burst through
it. The same fact, on a grander scale, has been remarked in
the eastern and loftiest line of the Bolivian Cordillera,
through which the rivers pass: analogous facts have also
been observed in other quarters of the world. On the sup-
position of the subsequent and gradual elevation of the Por-
tillo line, this can be understood; for a chain of islets would
at first appear, and, as these were lifted up, the tides would be
always wearing deeper and broader channels between them.
THE VOYAGE OF THE BEAGLE 341
At the present day, even in the most retired Sounds on the
coast of Tierra del Fuego, the currents in the transverse
breaks which connect the longitudinal channels, are very
strong, so that in one transverse channel even a small vessel
under sail was whirled round and round.
About noon we began the tedious ascent of the Peuquenes
ridge, and then for the first time experienced some little
difficulty in our respiration. The mules would halt every fifty
yards, and after resting for a few seconds the poor willing
animals started of their own accord again. The short breath-
ing from the rarefied atmosphere is called by the Chilenos
" puna ;" and they have most ridiculous notions concerning
its origin. Some say " all the waters here have puna ;" others
that " where there is snow there is puna ;" — and this no
doubt is true. The only sensation I experienced was a slight
tightness across the head and chest, like that felt on leaving
a warm room and running quickly in frosty weather. There
was some imagination even in this ; for upon finding fossil
shells on the highest ridge, I entirely forgot the puna in my
delight. Certainly the exertion of walking was extremely
great, and the respiration became deep and laborious : I am
told that in Potosi (about 13,000 feet above the sea) strangers
do not become thoroughly accustomed to the atmosphere for
an entire year. The inhabitants all recommend onions for
the puna; as this vegetable has sometimes been given in
Europe for pectoral complaints, it may possibly be of real
service: — for my part I found nothing so good as the fossil
shells !
When about half-way up we met a large party with sev-
enty loaded mules. It was interesting to hear the wild cries
of the muleteers, and to watch the long descending string
of the animals; they appeared so diminutive, there being
nothing but the black mountains with which they could be
compared. When near the summit, the wind, as generally
happens, was impetuous and extremely cold. On each side of
the ridge, we had to pass over broad bands of perpetual
snow, which were now soon to be covered by a fresh layer.
When we reached the crest and looked backwards, a glorious
view was presented. The atmosphere resplendently clear;
342 CHARLES DARWIN
the sky an intense blue; the profound valleys; the wild
broken forms; the heaps of ruins, piled up during the lapse
of ages; the bright-coloured rocks, contrasted with the quiet
mountains of snow; all these together produced a scene no
one could have imagined. Neither plant nor bird, excepting
a few condors wheeling around the higher pinnacles, dis-
tracted my attention from the inanimate mass. I felt glad
that I was alone: it was like watching a thunderstorm, or
hearing in full orchestra a chorus of the Messiah.
On several patches of the snow I found the Protococcus
nivalis, or red snow, so well known from the accounts of
Arctic navigators. My attention was called to it, by observ-
ing the footsteps of the mules stained a pale red, as if their
hoofs had been slightly bloody. I at first thought that it was
owing to dust blown from the surrounding mountains of red
porphyry; for from the magnifying power of the crystals
of snow, the groups of these microscopical plants appeared
like coarse particles. The snow was coloured only where it
had thawed very rapidly, or had been accidentally crushed.
A little rubbed on paper gave it a faint rose tinge mingled
with a little brick-red. I afterwards scraped some off the
paper, and found that it consisted of groups of little spheres
in colourless cases, each of the thousandth part of an inch in
diameter.
The wind on the crest of the Peuquenes, as just remarked,
is generally impetuous and very cold: it is said 3 to blow
steadily from the westward or Pacific side. As the observa-
tions have been chiefly made in summer, this wind must be
an upper and return current. The Peak of Teneriffe, with
a less elevation, and situated in lat. 28 . in like manner falls
within an upper return stream. At first it appears rather
surprising, that the trade-wind along the northern parts of
Chile and on the coast of Peru, should blow in so very south-
erly a direction as it does ; but when we reflect that the Cor-
dillera, running in a north and south line, intercepts, like a
great wall, the entire depth of the lower atmospheric current,
we can easily see that the trade-wind must be drawn north-
ward, following the line of mountains, towards the equatorial
3 Dr. Gillies in Journ. of Nat. and Geograph. Science, Aug., 1830. This
author gives the heights of the Passes.
THE VOYAGE OF THE BEAGLE 343
regions, and thus lose part of that easterly movement which
it otherwise would have gained from the earth's rotation. At
Mendoza, on the eastern foot of the Andes, the climate is
said to be subject to long calms, and to frequent though false
appearances of gathering rain-storms: we may imagine that
the wind, which coming from the eastward is thus banked up
by the line of mountains, would become stagnant and irregu-
lar in its movements.
Having crossed the Peuquenes, we descended into a moun-
tainous country, intermediate between the two main ranges,
and then took up our quarters for the night. We were now
in the republic of Mendoza. The elevation was probably not
under 11,000 feet, and the vegetation in consequence exceed-
ingly scanty. The root of a small scrubby plant served as
fuel, but it made a miserable fire, and the wind was
piercingly cold. Being quite tired with my day's work, I
made up my bed as quickly as I could, and went to sleep.
About midnight I observed the sky became suddenly clouded :
I awakened the arriero to know if there was any danger of
bad weather ; but he said that without thunder and lightning
there was no risk of a heavy snow-storm. The peril is
imminent, and the difficulty of subsequent escape great, to
any one overtaken by bad weather between the two ranges.
A certain cave offers the only place of refuge: Mr. Cald-
cleugh, who crossed on this same day of the month, was
detained there for some time by a heavy fall of snow. Casu-
chas, or houses of refuge, have not been built in this pass
as in that of Uspallata, and, therefore, during the autumn,
the Portillo is little frequented. I may here remark that
within the main Cordillera rain never falls, for during the
summer the sky is cloudless, and in winter snow-storms alone
occur.
At the place where we slept water necessarily boiled, from
the diminished pressure of the atmosphere, at a lower tem-
perature than it does in a less lofty country; the case being
the converse of that of a Papin's digester. Hence the pota-
toes, after remaining for some hours in the boiling water,
were nearly as hard as ever. The pot was left on the fire
all night, and next morning it was boiled again, but yet the
potatoes were not cooked. I found out this, by overhearing
344 CHARLES DARWIN
my two companions discussing the cause; they had come
to the simple conclusion, " that the cursed pot [which was a
new one] did not choose to boil potatoes. "
March 22nd. — After eating our potatoless breakfast, we
travelled across the intermediate tract to the foot of the
Portillo range. In the middle of summer cattle are brought
up here to graze ; but they had now all been removed : even
the greater number of the Guanacos had decamped, knowing
well that if overtaken here by a snow-storm, they would be
caught in a trap. We had a fine view of a mass of moun-
tains called Tupungato, the whole clothed with unbroken
snow, in the midst of which there was a blue patch, no
doubt a glacier; — a circumstance of rare occurrence in these
mountains. Now commenced a heavy and long climb, simi-
lar to that of the Peuquenes. Bold conical hills of red
granite rose on each hand ; in the valleys there were several
broad fields of perpetual snow. These frozen masses, during
the process of thawing, had in some parts been converted
into pinnacles or columns, 4 which, as they were high and
close together, made it difficult for the cargo mules to pass.
On one of these columns of ice, a frozen horse was stick-
ing as on a pedestal, but with its hind legs straight up in
the air. The animal, I suppose, must have fallen with its
head downward into a hole, when the snow was continuous,
and afterwards the surrounding parts must have been
removed by the thaw.
When nearly on the crest of the Portillo, we were envel-
oped in a falling cloud of minute frozen spicula. This was
very unfortunate, as it continued the whole day, and quite
intercepted our view. The pass takes its name of Portillo,
from a narrow cleft or doorway on the highest ridge,
through which the road passes. From this point, on a clear
day, those vast plains which uninterruptedly extend to the
Atlantic Ocean can be seen. We descended to the upper
4 This structure in frozen snow was long since observed by Scoresby in
the icebergs near Spitzbergen, and, lately, with more care, by Colonel
Jackson (Journ. of Geograph. Soc, vol. v. p. 12) on the Neva. Mr. Lyell
(Principles, vol. iv. p. 360) has compared the fissures by which the
columnar structure seems to be determined, to the joints that traverse
nearly all rocks, but which are best seen in the non-stratified masses. I
may observe, that in the case of the frozen snow, the columnar structure
must be owing to a " metamorphic " action, and not to a process during
deposition.
THE VOYAGE OF THE BEAGLE 345
limit of vegetation, and found good quarters for the night
under the shelter of some large fragments of rock. We met
here some passengers, who made anxious inquiries about the
state of the road. Shortly after it was dark the clouds sud-
denly cleared away, and the effect was quite magical. The
great mountains, bright with the full moon, seemed impend-
ing over us on all sides, as over a deep crevice : one morn-
ing, very early, I witnessed the same striking effect. As
soon as the clouds were dispersed it froze severely; but as
there was no wind, we slept very comfortably.
The increased brilliancy of the moon and stars at this
elevation, owing to the perfect transparency of the atmos-
phere, was very remarkable. Travelers having observed
the difficulty of judging heights and distances amidst lofty
mountains, have generally attributed it to the absence of
objects of comparison. It appears to me, that it is fully as
much owing to the transparency of the air confounding
objects at different distances, and likewise partly to the
novelty of an unusual degree of fatigue arising from a little
exertion, — habit being thus opposed to the evidence of the
senses. I am sure that this extreme clearness of the air
gives a peculiar character to the landscape, all objects
appearing to be brought nearly into one plane, as in a draw-
ing or panorama. The transparency is, I presume, owing to
the equable and high state of atmospheric dryness. This
dryness was shown by the manner in which woodwork
shrank (as I soon found by the trouble my geological ham-
mer gave me) ; by articles of food, such as bread and sugar,
becoming extremely hard; and by the preservation of the
skin and parts of the flesh of the beasts, which had perished
on the road. To the same cause we must attribute the singu-
lar facility with which electricity is excited. My flannel
waistcoat, when rubbed in the dark, appeared as if it had
been washed with phosphorus; — every hair on a dog's back
crackled; — even the linen sheets, and leathern straps of the
saddle, when handled, emitted sparks.
March 23rd. — The descent on the eastern side of the Cor-
dillera is much shorter or steeper than on the Pacific side;
in other words, the mountains rise more abruptly from the
plains than from the alpine country of Chile. A level and
346 CHARLES DARWIN
brilliantly white sea of clouds was stretched out beneath our
feet, shutting out the view of the equally level Pampas. We
soon entered the band of clouds, and did not again emerge
from it that day. About noon, finding pasture for the ani-
mals and bushes for firewood at Los Arenales, we stopped
for the night. This was near the uppermost limit of bushes,
and the elevation, I suppose, was between seven and eight
thousand feet.
I was much struck with the marked difference between
the vegetation of these eastern valleys and those on the
Chilian side: yet the climate, as well as the kind of soil, is
nearly the same, and the difference of longitude very trifling.
The same remark holds good with the quadrupeds, and in
a lesser degree with the birds and insects. I may instance the
mice, of which I obtained thirteen species on the shores of
the Atlantic, and five on the Pacific, and not one of them
is identical. We must except all those species, which habitu-
ally or occasionally frequent elevated mountains; and cer-
tain birds, which range as far south as the Strait of Magel-
lan. This fact is in perfect accordance with the geological
history of the Andes; for these mountains have existed as
a great barrier since the present races of animals have
appeared; and therefore, unless we suppose the same species
to have been created in two different places, we ought not to
expect any closer similarity between the organic beings on
the opposite sides of the Andes than on the opposite shores
of the ocean. In both cases, we must leave out of the ques-
tion those kinds which have been able to cross the barrier,
whether of solid rock or salt-water. 5
A great number of the plants and animals were absolutely
the same as, or most closely allied to, those of Patagonia.
We here have the agouti, bizcacha, three species of arma-
dillo, the ostrich, certain kinds of partridges and other birds,
none of which are ever seen in Chile, but are the character-
istic animals of the desert plains of Patagonia. We have
likewise many of the same (to the eyes of a person who is
5 This is merely an illustration of the admirable laws, first laid down
by Mr. Lyell, on the geographical distribution of animals, as influenced
by geological changes. The whole reasoning, of course, is founded on the
assumption of the immutability of species; otherwise the difference in the
species in the two regions might be considered as superinduced during a
length of time.
THE VOYAGE OF THE BEAGLE 347
not a botanist) thorny stunted bushes, withered grass, and
dwarf plants. Even the black slowly crawling beetles are
closely similar, and some, I believe, on rigorous examination,
absolutely identical. It had always been to me a subject of
regret, that we were unavoidably compelled to give up the
ascent of the S. Cruz river before reaching the mountains:
I always had a latent hope of meeting with some great
change in the features of the country; but I now feel sure,
that it would only have been following the plains of Pata-
gonia up a mountainous ascent.
March 24th. — Early in the morning I climbed up a moun-
tain on one side of the valley, and enjoyed a far extended
view over the Pampas. This was a spectacle to which I had
always looked forward with interest, but I was disappointed :
at the first glance it much resembled a distant view of the
ocean, but in the northern parts many irregularities were
soon distinguishable. The most striking feature consisted
in the rivers, which, facing the rising sun, glittered like
silver threads, till lost in the immensity of the distance. At
midday we descended the valley, and reached a hovel, where
an officer and three soldiers were posted to examine pass-
ports. One of these men was a thoroughbred Pampas
Indian: he was kept much for the same purpose as a blood-
hound, to track out any person who might pass by secretly,
either on foot or horseback. Some years ago, a passenger
endeavoured to escape detection, by making a long circuit
over a neighbouring mountain; but this Indian, having by
chance crossed his track, followed it for the whole day over
dry and very stony hills, till at last he came on his prey
hidden in a gully. We here heard that the silvery clouds,
which we had admired from the bright region above, had
poured down torrents of rain. The valley from this point
gradually opened, and the hills became mere water-worn
hillocks compared to the giants behind: it then expanded
into a gently sloping plain of shingle, covered with low trees
and bushes. This talus, although appearing narrow, must be
nearly ten miles wide before it blends into the apparently
dead level Pampas. We passed the only house in this neigh-
bourhood, the Estancia of Chaquaio ; and at sunset we pulled
up in the first snug corner, and there bivouacked.
348 CHARLES DARWIN
March 25th. — I was reminded of the Pampas of Buenos
Ayres, by seeing the disk of the rising sun, intersected by an
horizon level as that of the ocean. During the night a heavy
dew fell, a circumstance which we did not experience within
the Cordillera. The road proceeded for some distance due
east across a low swamp; then meeting the dry plain, it
turned to the north towards Mendoza. The distance is two
very long days' journey. Our first day's journey was called
fourteen leagues to Estacado, and the second seventeen to
Luxan, near Mendoza. The whole distance is over a level
desert plain, with not more than two or three houses. The
sun was exceedingly powerful, and the ride devoid of all
interest. There is very little water in this " traversia," and
in our second day's journey we found only one little pool.
Little water flows from the mountains, and it soon becomes
absorbed by the dry and porous soil; so that, although we
travelled at the distance of only ten or fifteen miles from
the outer range of the Cordillera, we did not cross a single
stream. In many parts the ground was incrusted with a
saline efflorescence; hence we had the same salt-loving
plants which are common near Bahia Blanca. The land-
scape has a uniform character from the Strait of Magellan,
along the whole eastern coast of Patagonia, to the Rio Colo-
rado; and it appears that the same kind of country extends
inland from this river, in a sweeping line as far as San Luis,
and perhaps even further north. To the eastward of this
curved line lies the basin of the comparatively damp and
green plains of Buenos Ayres. The sterile plains of Men-
doza and Patagonia consist of a bed of shingle, worn smooth
and accumulated by the waves of the sea ; while the Pampas,
covered by thistles, clover, and grass, have been formed by
the ancient estuary mud of the Plata.
After our two days' tedious journey, it was refreshing to
see in the distance the rows of poplars and willows growing
round the village and river of Luxan. Shortly before we
arrived at this place, we observed to the south a ragged cloud
of dark reddish-brown colour. At first we thought that it
was smoke from some great fire on the plains; but we soon
found that it was a swarm of locusts. They were flying
northward; and with the aid of a light breeze, they overtook
THE VOYAGE OF THE BEAGLE 349
us at a rate of ten or fifteen miles an hour. The main body
filled the air from a height of twenty feet, to that, as it ap-
peared, of two or three thousand above the ground ; " and the
sound of their wings was as the sound of chariots of many
horses running to battle:" or rather, I should say, like a
strong breeze passing through the rigging of a ship. The
sky, seen through the advanced guard, appeared like a mezzo-
tinto engraving, but the main body was impervious to sight;
they were not, however, so thick together, but that they
could escape a stick waved backwards and forwards. When
they alighted, they were more numerous than the leaves in
the field, and the surface became reddish instead of being
green : the swarm having once alighted, the individuals flew
from side to side in all directions. Locusts are not an un-
common pest in this country : already during the season, sev-
eral smaller swarms had come up from the south, where, as
apparently in all other parts of the world, they are bred in
the deserts. The poor cottagers in vain attempted by light-
ing fires, by shouts, and by waving branches to avert the
attack. This species of locust closely resembles, and perhaps
is identical with, the famous Gryllus migratorius of the East.
We crossed the Luxan, which is a river of considerable
size, though its course towards the sea-coast is very imper-
fectly known : it is .even doubtful whether, in passing over
the plains, it is not evaporated and lost. We slept in the
village of Luxan, which is a small place surrounded by gar-
dens, and forms the most southern cultivated district in the
Province of Mendoza; it is five leagues south of the capital.
At night I experienced an attack (for it deserves no less a
name) of the Benchuca, a species of Reduvius, the great
black bug of the Pampas. It is most disgusting to feel soft
wingless insects, about an inch long, crawling over one's
body. Before sucking they are quite thin, but afterwards
they become round and bloated with blood, and in this state
are easily crushed. One which I caught at Iquique, (for they
are found in Chile and Peru,) was very empty. When placed
on a table, and though surrounded by people, if a finger was
presented, the bold insect would immediately protrude its
sucker, make a charge, and if allowed, draw blood. No pain
was caused by the wound. It was curious to watch its body
350 CHARLES DARWIN
during the act of sucking, as in less than ten minutes it
changed from being as flat as a wafer to a globular form.
This one feast, for which the benchuca was indebted to one
of the officers, kept it fat during four whole months; but,
after the first fortnight, it was quite ready to have another
suck.
March 27th. — We rode on to Mendoza. The country was
beautifully cultivated, and resembled Chile. This neighbour-
hood is celebrated for its fruit; and certainly nothing could
appear more flourishing than the vineyards and the orchards
of figs, peaches, and olives. We bought water-melons nearly
twice as large as a man's head, most deliciously cool and
well-flavoured, for a halfpenny apiece; and for the value of
threepence, half a wheelbarrowful of peaches. The culti-
vated and enclosed part of this province is very small; there
is little more than that which we passed through between
Luxan and the capital. The land, as in Chile, owes its fer-
tility entirely to artificial irrigation ; and it is really wonder-
ful to observe how extraordinarily productive a barren
traversia is thus rendered.
We stayed the ensuing day in Mendoza. The prosperity
of the place has much declined of late years. The inhabit-
ants say " it is good to live in, but very bad to grow rich in."
The lower orders have the lounging, reckless manners of the
Gauchos of the Pampas; and their dress, riding-gear, and
habits of life, are nearly the same. To my mind the town
had a stupid, forlorn aspect. Neither the boasted alameda,
nor the scenery, is at all comparable with that of Santiago;
but to those who, coming from Buenos Ayres, have just
crossed the unvaried Pampas, the gardens and orchards must
appear delightful. Sir F. Head, speaking of the inhabitants,
says, " They eat their dinners, and it is so very hot, they go
to sleep — and could they do better ? " I quite agree with
Sir F. Head: the happy doom of the Mendozinos is to eat,
sleep and be idle.
March 2pth. — We set out on our return to Chile, by the
Uspallata pass situated north of Mendoza. We had to cross
a long and most sterile traversia of fifteen leagues. The
soil in parts was absolutely bare, in others covered by num-
THE VOYAGE OF THE BEAGLE 351
berless dwarf cacti, armed with formidable spines, and called
by the inhabitants " little lions." There were, also, a few
low bushes. Although the plain is nearly three thousand feet
above the sea, the sun was very powerful; and the heat, as
well as the clouds of impalpable dust, rendered the travelling
extremely irksome. Our course during the day lay nearly
parallel to the Cordillera, but gradually approaching them.
Before sunset we entered one of the wide valleys, or rather
bays, which open on the plain: this soon narrowed into a
ravine, where a little higher up the house of Villa Vicencio
is situated. As we had ridden all day without a drop of
water, both our mules and selves were very thirsty, and we
looked out anxiously for the stream which flows down this
valley. It was curious to observe how gradually the water
made its appearance : on the plain the course was quite dry ;
by degrees it became a little damper; then puddles of water
appeared ; these soon became connected ; and at Villa Vicen-
cio there was a nice little rivulet.
20th. — The solitary hovel which bears the imposing name
of Villa Vicencio, has been mentioned by every traveller who
has crossed the Andes. I stayed here and at some neigh-
bouring mines during the two succeeding days. The geology
of the surrounding country is very curious. The Uspallata
range is separated from the main Cordillera by a long nar-
row plain or basin, like those so often mentioned in Chile,
but higher, being six thousand feet above the sea. This
range has nearly the same geographical position with respect
to the Cordillera, which the gigantic Portillo line has, but it
is of a totally different origin: it consists of various kinds of
submarine lava, alternating with volcanic sandstones and
other remarkable sedimentary deposits; the whole having a
very close resemblance to some of the tertiary beds on the
shores of the Pacific. From this resemblance I expected to
find silicified wood, which is generally characteristic of those
formations. I was gratified in a very extraordinary manner.
In the central part of the range, at an elevation of about
seven thousand feet, I observed on a bare slope some snow-
white projecting columns. These were petrified trees, eleven
being silicified, and from thirty to forty converted into
coarsely-crystallized white calcareous spar. They were ab-
352 CHARLES DARWIN
rnptly broken off, the upright stumps projecting a few feet
above the ground. The trunks measured from three to five
feet each in circumference. They stood a little way apart
from each other, but the whole formed one group. Mr. Rob-
ert Brown has been kind enough to examine the wood: he
says it belongs to the fir tribe, partaking of the character
of the Araucarian family, but with some curious points of
affinity with the yew. The volcanic sandstone in which the
trees were embedded, and from the lower part of which they
must have sprung, had accumulated in successive thin layers
around their trunks; and the stone yet retained the impres-
sion of the bark.
It required little geological practice to interpret the mar-
vellous story which this scene at once unfolded; though I
confess I was at first so much astonished that I could
scarcely believe the plainest evidence. I saw the spot where
a cluster of fine trees once waved their branches on the
shores of the Atlantic, when that ocean (now driven back
700 miles) came to the foot of the Andes. I saw that they
had sprung from a volcanic soil which had been raised above
the level of the sea, and that subsequently this dry land,
with its upright trees, had been let down into the depths of
the ocean. In these depths, the formerly dry land was
covered by sedimentary beds, and these again by enormous
streams of submarine lava — one such mass attaining the
thickness of a thousand feet; and these deluges of molten
stone and aqueous deposits five times alternately had been
spread out. The ocean which received such thick masses,
must have been profoundly deep ; but again the subterranean
forces exerted themselves, and I now beheld the bed of
that ocean, forming a chain of mountains more than seven
thousand feet in height. Nor had those antagonistic forces
been dormant, which are always at work wearing down the
surface of the land; the great piles of strata had been in-
tersected by many wide valleys, and the trees now changed
into silex, were exposed projecting from the volcanic soil,
now changed into rock, whence formerly, in a green and
budding state, they had raised their lofty heads. Now,
all is utterly irreclaimable and desert; even the lichen can-
not adhere to the stony casts of former trees. Vast, and
THE VOYAGE OF THE BEAGLE 353
scarcely comprehensible as such changes must ever appear,
yet they have all occurred within a period, recent when
compared with the history of the Cordillera; and the Cor-
dillera itself is absolutely modern as compared with many
of the fossiliferous strata of Europe and America.
April ist. — We crossed the Upsallata range, and at night
slept at the custom-house — the. only inhabited spot on the
plain. Shortly before leaving the mountains, there was a
very extraordinary view; red, purple, green, and quite white
sedimentary rocks, alternating with black lavas, were broken
up and thrown into all kinds of disorder by masses of por-
phyry of every shade of colour, from dark brown to the
brightest lilac. It was the first view I ever saw, which
really resembled those pretty sections which geologists make
of the inside of the earth.
The next day we crossed the plain, and followed the course
of the same great mountain stream which flows by Luxan.
Here it was a furious torrent, quite impassable, and appeared
larger than in the low country, as was the case with the rivu-
let of Villa Vicencio. On the evening of the succeeding day,
we reached the Rio de las Vacas, which is considered the
worst stream in the Cordillera to cross. As all these rivers
have a rapid and short course, and are formed by the melting
of the snow, the hour of the day makes a considerable differ-
ence in their volume. In the evening the stream is muddy
and full, but about daybreak it becomes clearer, and much
less impetuous. This we found to be the case with the Rio
Vacas, and in the morning we crossed it with little difficulty.
The scenery thus far was very uninteresting, compared
with that of the Portillo pass. Little can be seen beyond the
bare walls of the one grand flat-bottomed valley, which the
road follows up to the highest crest. The valley and
the huge rocky mountains are extremely barren: during the
two previous nights the poor mules had absolutely nothing
to eat, for excepting a few low resinous bushes, scarcely a
plant can be seen. In the course of this day we crossed some
of the worst passes in the Cordillera, but their danger has
been much exaggerated. I was told that if I attempted to
pass on foot,, my head would turn giddy, and that there was
no room to dismount; but I did not see a place where any
VOL. XX IX — L HC
354 CHARLES DARWIN
one might not have walked over backwards, or got off his
mule on either side. One of the bad passes, called las
Animas (the souls), I had crossed, and did not find out
till a day afterwards, that it was one of the awful dangers.
No doubt there are many parts in which, if the mule should
stumble, the rider would be hurled down a great precipice;
but of this there is little chance. I dare say, in the spring,
the " laderas," or roads, which each year are formed anew
across the piles of fallen detritus, are very bad; but from
what I saw, I suspect the real danger is nothing. With
cargo-mules the case is rather different, for the loads pro-
ject so far, that the animals, occasionally running against
each other, or against a point of rock, lose their balance, and
are thrown down the precipices. In crossing the rivers
I can well believe that the difficulty may be very great: at
this season there was little trouble, but in the summer they
must be very hazardous. I can quite imagine, as Sir F.
Head describes, the different expressions of those who have
passed the gulf, and those who are passing. I never heard
of any man being drowned, but with loaded mules it fre-
quently happens. The arriero tells you to show your mule
the best line, and then allow her to cross as she likes: the
cargo-mule takes a bad line, and is often lost.
April 4th. — From the Rio de las Vacas to the Puente del
Incas, half a day's journey. As there was pasture for the
mules, and geology for me, we bivouacked here for the
night. When one hears of a natural Bridge, one pictures
to one's self some deep and narrow ravine, across which a
bold mass of rock has fallen; or a great arch hollowed out
like the vault of a cavern. Instead of this, the Incas
Bridge consists of a crust of stratified shingle cemented to-
gether by the deposits of the neighbouring hot springs. It
appears, as if the stream had scooped out a channel on one
side, leaving an overhanging ledge, which was met by earth
and stones falling down from the opposite cliff. Certainly
an oblique junction, as would happen in such a case, was
very distinct on one side. The Bridge of the Incas is by
no means worthy of the great monarchs whose name it
bears.
5th. — We had a long day's ride across the central ridge,
THE VOYAGE OF THE BEAGLE 355
from the Incas Bridge to the Ojos del Agua, which are situ-
ated near the lowest casucha on the Chilian side. These
casuchas are round little towers, with steps outside to reach
the floor, which is raised some feet above the ground on ac-
count of the snow-drifts. They are eight in number, and
under the Spanish government were kept during the winter
well stored with food and charcoal, and each courier had a
master-key. Now they only answer the purpose of caves, or
rather dungeons. Seated on some little eminence, they are
not, however, ill suited to the surrounding scene of desola-
tion. The zigzag ascent of the Cumbre, or the partition of
the waters, was very steep and tedious; its height, according
to Mr. Pentland, is 12,454 ^ eet - The road did not pass over
any perpetual snow, although there were patches of it on
both hands. The wind on the summit was exceedingly cold,
but it was impossible not to stop for a few minutes to ad-
mire, again and again, the colour of the heavens, and the
brilliant transparency of the atmosphere. The scenery was
grand: to the westward there was a fine chaos of mountains,
divided by profound ravines. Some snow generally falls be-
fore this period of the season, and it has even happened that
the Cordillera have been finally closed by this time. But
we were most fortunate. The sky, by night and by day, was
cloudless, excepting a few round little masses of vapour, that
floated over the highest pinnacles. I have often seen these
islets in the sky, marking the position of the Cordillera,
when the far-distant mountains have been hidden beneath
the horizon.
April 6th. — In the morning we found some thief had
stolen one of our mules, and the bell of the madrina. We
therefore rode only two or three miles down the valley, and
stayed there the ensuing day in hopes of recovering the mule,
which the arriero thought had been hidden in some ravine.
The scenery in this part had assumed a Chilian character:
the lower sides of the mountains, dotted over with the pale
evergreen Quillay tree, and with the great chandelier-like
cactus, are certainly more to be admired than the bare east-
ern valleys; but I cannot quite agree with the admiration
expressed by some travellers. The extreme pleasure, I sus-
pect, is chiefly owing to the prospect of a good fire and of a
356 CHARLES DARWIN
good supper, after escaping from the cold regions above : and
I am sure I most heartily participated in these feelings.
8th. — We left the valley of the Aconcagua, by which we
had descended, and reached in the evening a cottage near the
Villa del St. Rosa. The fertility of the plain was delight-
ful: the autumn being advanced, the leaves of many of the
fruit-trees were falling; and of the labourers, — some were
busy in drying figs and peaches on the roofs of their cot-
tages, v/hile others were gathering the grapes from the vine-
yards. It was a pretty scene ; but I missed that pensive still-
ness which makes the autumn in England indeed the evening
of the year. On the ioth we reached Santiago, where I re-
ceived a very kind and hospitable reception from Mr. Cald-
cleugh. My excursion only cost me twenty-four days, and
never did I more deeply enjoy an equal space of time. A
few days afterwards I returned to Mr. Cor field's house at
Valparaiso.
CHAPTER XVI
Northern Chile and Peru
Coast-road to Coquimbo — Great Loads carried by the Miners — Co-
quimbo — Earthquake — Step-formed Terraces — Absence of recent
Deposits — Contemporaneousness of the Tertiary Formations —
Excursion up the Valley — Road to Guasco — Deserts — Valley of
Copiapo — Rain and Earthquakes — Hydrophobia — The Despoblado
— Indian Ruins — Probable Change of Climate — River-bed arched
by an Earthquake — Cold Gales of Wind — Noises from a Hill —
Iquique — Salt Alluvium — Nitrate of Soda — Lima — Unhealthy
Country — Ruins of Callao, overthrown by an Earthquake — Recent
subsidence — Elevated Shells on San Lorenzo, their decomposition —
Plain with embedded Shells and fragments of Pottery — Antiquity
of the Indian Race.
APRIL 27th. — I set out on a journey to Coquimbo, and
jL-M thence through Guasco to Copiapo, where Captain
Fitz Roy kindly offered to pick me up in the Beagle.
The distance in a straight line along the shore northward is
only 420 miles; but my mode of travelling made it a very
long journey. L bought four horses and two mules, the
latter carrying the luggage on alternate days. The six
animals together only cost the value of twenty-five pounds
sterling, and at Copiapo I sold them again for twenty-three.
We travelled in the same independent manner as before,
cooking our own meals, and sleeping in the open air. As
we rode towards the Vino del Mar, I took a farewell view
of Valparaiso, and admired its picturesque appearance. For
geological purposes I made a detour from the high road
to the foot of the Bell of Quillota. We passed through an
alluvial district rich in gold, to the neighbourhood of Li-
mache, where we slept. Washing for gold supports the in-
habitants of numerous hovels, scattered along the sides of
each little rivulet; but, like all those whose gains are un-
certain, they are unthrifty in all their habits, and con-
sequently poor.
357
358 CHARLES DARWIN
28th. — In the afternoon we arrived at a cottage at the
foot of the Bell mountain. The inhabitants were freehold-
ers, which is not very usual in Chile. They supported them-
selves on the produce of a garden and a little field, but were
very poor. Capital is here so deficient, that the people are
obliged to sell their green corn while standing in the field,
in order to buy necessaries for the ensuing year. Wheat in
consequence was dearer in the very district of its production
than at Valparaiso, where the contractors live. The next
day we joined the main road to Coquimbo. At night there
was a very light shower of rain : this was the first drop that
had fallen since the heavy rain of September nth and 12th,
which detained me a prisoner at the Baths of Cauquenes.
The interval was seven and a half months; but the rain this
year in Chile was rather later than usual. The distant Andes
were now covered by a thick mass of snow, and were a glo-
rious sight.
May 2nd. — The road continued to follow the coast, at no
great distance from the sea. The few trees and bushes which
are common in central Chile decreased rapidly in numbers,
and were replaced by a tall plant, something like a yucca in
appearance. The surface of the country, on a small scale,
was singularly broken and irregular; abrupt little peaks of
rock rising out of small plains or basins. The indented coast
and the bottom of the neighbouring sea, studded with break-
ers, would, if converted into dry land, present similar forms ;
and such a conversion without doubt has taken place in the
part over which we rode.
3rd. — Quilimari to Conchalee. The country became more
and more barren. In the valleys there was scarcely sufficient
water for any irrigation; and the intermediate land was
quite bare, not supporting even goats. In the spring, after
the winter showers, a thin pasture rapidly springs up, and
cattle are then driven down from the Cordillera to graze
for a short time. It is curious to observe how the seeds of
the grass and other plants seem to accommodate themselves,
as if by an acquired habit, to the quantity of rain which
falls upon different parts of this coast. One shower far
northward at Copiapo produces as great an effect on the
vegetation, as two at Guasco, and three or four in this
THE VOYAGE OF THE BEAGLE 359
district. At Valparaiso a winter so dry as greatly to injure
the pasture, would at Guasco produce the most unusual
abundance. Proceeding northward, the quantity of rain does
not appear to decrease in strict proportion to the latitude.
At Conchalee, which is only 67 miles north of Valparaiso,
rain is not expected till the end of May; whereas at Val-
paraiso some generally falls early in April : the annual quan-
tity is likewise small in proportion to the lateness of the
season at which it commences.
4th. — Finding the coast-road devoid of interest of any
kind, we turned inland towards the mining district and
valley of Illapel. This valley, like every other in Chile, is
level, broad, and very fertile: it is bordered on each side,
either by cliffs of stratified shingle, or by bare rocky moun-
tains. Above the straight line of the uppermost irrigating
ditch, all is brown as on a high road; while all below is of as
bright a green as verdigris, from the beds of alfalfa, a kind
of clover. We proceeded to Los Hornos, another mining
district, where the principal hill was drilled with holes, like
a great ants'-nest. The Chilian miners are a peculiar race
of men in their habits. Living for weeks together in the
most desolate spots, when they descend to the villages on
feast-days, there is no excess of extravagance into which
they do not run. ' They sometimes gain a considerable sum,
and then, like sailors with prize-money, they try how soon
they can contrive to squander it. They drink excessively,
buy quantities of clothes, and in a few days return penniless
to their miserable abodes, there to work harder than beasts
of burden. This thoughtlessness, as with sailors, is evidently
the result of a similar manner of life. Their daily food is
found them, and they acquire no habits of carefulness: more-
over, temptation and the means of yielding to it are placed
in their power at the same time. On the other hand, in
Cornwall, and some other parts of England, where the sys-
tem of selling part of the vein is followed, the miners, from
being obliged to act and think for themselves, are a singu-
larly intelligent and well-conducted set of men.
The dress of the Chilian miner is peculiar and rather
picturesque. He wears a very long shirt of some dark-col-
oured baize, with a leathern apron ; the whole being fastened
360 CHARLES DARWIN
round his waist by a bright-coloured sash. His trousers are
very broad, and his small cap of scarlet cloth is made to fit
the head closely. We met a party of these miners in full
costume, carrying the body of one of their companions to be
buried. They marched at a very quick trot, four men sup-
porting the corpse. One set having run as hard as they
could for about two hundred yards, were relieved by four
others, who had previously dashed on ahead on horseback.
Thus they proceeded, encouraging each other by wild cries:
altogether the scene formed a most strange funeral.
We continued travelling northward, in a zigzag line;
sometimes stopping a day to geologize. The country was so
thinly inhabited, and the track so obscure, that we often had
difficulty in finding our way. On the 12th I stayed at some
mines. The ore in this case was not considered particularly
good, but from being abundant it was supposed the mine
would sell for about thirty or forty thousand dollars (that is,
6000 or 8000 pounds sterling) ; yet it had been bought by
one of the English Associations for an ounce of gold (3/.
8s.). The ore is yellow pyrites, which, as I have already re-
marked, before the arrival of the English, was not supposed
to contain a particle of copper. On a scale of profits nearly
as great as in the above instance, piles of cinders, abounding
with minute globules of metallic copper, were purchased;
yet with these advantages, the mining associations, as is well
known, contrived to lose immense sums of money. The folly
of the greater number of the commissioners and shareholders
amounted to infatuation; — a thousand pounds per annum
given in some cases to entertain the Chilian authorities;
libraries of well-bound geological books ; miners brought out
for particular metals, as tin, which are not found in Chile;
contracts to supply the miners with milk, in parts where
there are no cows; machinery, where it could not possibly
be used; and a hundred similar arrangements, bore witness
to our absurdity, and to this day afford amusement to the
natives. Yet there can be no doubt, that the same capital
well employed in these mines would have yielded an im-
mense return, a confidential man of business, a practical
miner and assayer, would have been all that was required.
Captain Head has described the wonderful load which
THE VOYAGE OF THE BEAGLE 361
the " Apires," truly beasts of burden, carry up from the
deepest mines. I confess I thought the account exaggerated;
so that I was glad to take an opportunity of weighing one
of the loads, which I picked out by hazard. It required con-
siderable exertion on my part, when standing directly over
it, to lift it from the ground. The load was considered under
weight when found to be 197 pounds. The apire had car-
ried this up eighty perpendicular yards, — part of the way by
a steep passage, but the greater part up notched poles, placed
in a zigzag line up the shaft. According to the general
regulation, the apire is not allowed to halt for breath, ex-
cept the mine is six hundred feet deep. The average load is
considered as rather more than 200 pounds, and I have been
assured that one of 300 pounds (twenty-two stone and a half)
by way of a trial has been brought up from the deepest mine !
At this time the apires were bringing up the usual load
twelve times in the day; that is 2400 pounds from eighty
yards deep ; and they were employed in the intervals in break-
ing and picking ore.
These men, excepting from accidents, are healthy, and ap-
pear cheerful. Their bodies are not very muscular. They
rarely eat meat once a week, and never oftener, and then only
the hard dry charqui. Although with a knowledge that the
labour was voluntary, it was nevertheless quite revolting to
see the state in which they reached the mouth of the mine;
their bodies bent forward, leaning with their arms on the
steps, their legs bowed, their muscles quivering, the per-
spiration streaming from their faces over their breasts, their
nostrils distended, the corners of their mouth forcibly drawn
back, and the expulsion of their breath most laborious.
Each time they draw their breath, they utter an articulate
cry of " ay-ay," which ends in a sound rising from deep in
the chest, but shrill like the note of a fife. After staggering
to the pile of ore, they emptied the " carpacho ; " in two or
three seconds recovering their breath, they wiped the sweat
from their brows, and apparently quite fresh descended the
mine again at a quick pace. This appears to me a wonderful
instance of the amount of labour which habit, for it can be
nothing else, will enable a man to endure.
In the evening, talking with the mayor-domo of these
362 CHARLES DARWIN
mines about the number of foreigners now scattered over
the whole country, he told me that, though quite a young
man, he remembers when he was a boy at school at
Coquimbo, a holiday being given to see the captain of an
English ship, who was brought to the city to speak to the
governor. He believes that nothing would have induced
any boy in the school, himself included, to have gone close
to the Englishman; so deeply had they been impressed with
an idea of the heresy, contamination, and evil to be derived
from contact with such a person. To this day they relate
the atrocious actions of the bucaniers; «nd especially of
one man, who took away the figure of the Virgin Mary, and
returned the year after for that of St. Joseph, saying it
was a pity the lady should not have a husband. I heard
also of an old lady who, at a dinner at Coquimbo, remarked
how wonderfully strange it was that she should have lived
to dine in the same room with an Englishman; for she
remembered as a girl, that twice, at the mere cry of " Los
Ingleses," every soul, carrying what valuables they could,
had taken to the mountains.
14th. — We reached Coquimbo, where we stayed a few
days. The town is remarkable for nothing but its extreme
quietness. It is said to contain from 6000 to 8000 inhabitants.
On the morning of the 17th it rained lightly, the first time
this year, for about five hours. The farmers, who plant
corn near the sea-coast where the atmosphere is most humid,
taking advantage of this shower, would break up the ground ;
after a second they would put the seed in; and if a third
shower should fall, they would reap a good harvest in the
spring. It was interesting to watch the effect of this trifling
amount of moisture. Twelve hours afterwards the ground
appeared as dry as ever; yet after an interval of ten days,
all the hills were faintly tinged with green patches; the
grass being sparingly scattered in hair-like fibres a full
inch in length. Before this shower every part of the sur-
face was bare as on a high road.
In the evening, Captain Fitz Roy and myself were dining
with Mr. Edwards, an English resident well known for his
hospitality by all who have visited Coquimbo, when a sharp
earthquake happened. I heard the forecoming rumble, but
THE VOYAGE OF THE BEAGLE 363
from the screams of the ladies, the running of the servants,
and the rush of several of the gentlemen to the doorway, I
could not distinguish the motion. Some of the women after-
wards were crying with terror, and one gentleman said he
should not be able to sleep all night, or if he did, it would
only be to dream of falling houses. The father of this per-
son had lately lost all his property at Talcahuano, and he
himself had only just escaped a falling roof at Valparaiso,
in 1822. He mentioned a curious coincidence which then
happened: he was playing at cards, when a German, one of
the party, got up, and said he would never sit in a room in
these countries with the door shut, a? owing to his having
done so, he had nearly lost his life at Copiapo. Accordingly
he opened the door ; and no sooner had he done this, than he
cried out, " Here it comes again ! " and the famous shock
commenced. The whole party escaped. The danger in an
earthquake is not from the time lost in opening the door, but
from the chance of its becoming jammed by the movement
of the walls.
It is impossible to be much surprised at the fear which
natives and old residents, though some of them known to
be men of great command of mind, so generally experience
during earthquakes. I think, however, this excess of panic
may be partly attributed to a want of habit in governing
their fear, as it is not a feeling they are ashamed of. In-
deed, the natives do not like to see a person indifferent. I
heard of two Englishmen who, sleeping in the open air during
a smart shock, knowing that there was no danger, did not
rise. The natives cried out indignantly, " Look at those
heretics, they do not even get out of their beds! "
I spent some days in examining the step-formed terraces
of shingle, first noticed by Captain B. Hall, and believed
by Mr. Lyell to have been formed by the sea, during the
gradual rising of the land. This certainly is the true
explanation, for I found numerous shells of existing species
on these terraces. Five narrow, gently sloping, fringe-like
terraces rise one behind the other, and where best developed
are formed of shingle : they front the bay, and sweep up both
sides of the valley. At Guasco, north of Coquimbo, the phe-
364 CHARLES DARWIN
nomenon is displayed on a much grander scale, so as to
strike with surprise even some of the inhabitants. The ter-
races are there much broader, and may be called plains; in
some parts there are six of them, but generally only five;
they run up the valley for thirty-seven miles from the coast.
These step-formed terraces or fringes closely resemble those
in the valley of S. Cruz, and, except in being on a smaller
scale, those great ones along the whole coast-line of Pata-
gonia. They have undoubtedly been formed by the denud-
ing power of the sea, during long periods of rest in the
gradual elevation of the continent.
Shells of many existing species not only lie on the sur-
face of the terraces at Coquimbo (to a height of 250 feet),
but are embedded in a friable calcareous rock, which in some
places is as much as between twenty and thirty feet in thick-
ness, but is of little extent. These modern beds rest on an
ancient tertiary formation containing shells, apparently all
extinct. Although I examined so many hundred miles of
coast on the Pacific, as well as Atlantic side of the conti-
nent, I found no regular strata containing sea-shells of
recent species, excepting at this place, and at a few points
northward on the road to Guasco. This fact appears to me
highly remarkable; for the explanation generally given by
geologists, of the absence in any district of stratified fossil-
iferous deposits of a given period, namely, that the surface
then existed as dry land, is not here applicable; for we
know from the shells strewed on the surface and embedded
in loose sand or mould, that the land for thousands of miles
along both coasts has lately been submerged. The explana-
tion, no doubt, must be sought in the fact, that the whole
southern part of the continent has been for a long time
slowly rising; and therefore that all matter deposited along
shore in shallow water, must have been soon brought up
and slowly exposed to the wearing action of the sea-beach ;
and it is only in comparatively shallow water that the greater
number of marine organic beings can flourish, and in such
water it is obviously impossible that strata of any great
thickness can accumulate. To show the vast power of the
wearing action of sea-beaches, we need only appeal to the
great cliffs along the present coast of Patagonia, and to the
THE VOYAGE OF THE BEAGLE 365
escarpments or ancient sea-cliffs at different levels, one
above another, on that same line of coast.
The old underlying tertiary formation at Coquimbo,
appears to be of about the same age with several deposits
on the coast of Chile (of which that of Navedad is the
principal one), and with the great formation of Patagonia.
Both at Navedad and in Patagonia there is evidence, that
since the shells (a list of which has been seen by Professor
E. Forbes) there entombed were living, there has been a
subsidence of several hundred feet, as well as an ensuing
elevation. It may naturally be asked, how it comes that,
although no extensive fossiliferous deposits of the recent
period, nor of any period intermediate between it and the
ancient tertiary epoch, have been preserved on either side of
the continent, yet that at this ancient tertiary epoch, sedi-
mentary matter containing fossil remains, should have been
deposited and preserved at different points in north and
south lines, over a space of noo miles on the shores of the
Pacific, and of at least 1350 miles on the shores of the Atlan-
tic, and in an east and west line of 700 miles across the
widest part of the continent? I believe the explanation is
not difficult, and that it is perhaps applicable to nearly analo-
gous facts observed in other quarters of the world. Consid-
ering the enormous power of denudation which the sea
possesses, as shown by numberless facts, it is not probable
that a sedimentary deposit, when being upraised, could pass
through the ordeal of the beach, so as to be preserved in
sufficient masses to last to a distant period, without it were
originally of wide extent and of considerable thickness : now
it is impossible on a moderately shallow bottom, which
alone is favourable to most living creatures, that a thick
and widely extended covering of sediment could be spread
out, without the bottom sank down to receive the successive
layers. This seems to have actually taken place at about
the same period in southern Patagonia and Chile, though
these places are a thousand miles apart. Hence, if pro-
longed movements of approximately contemporaneous sub-
sidence are generally widely extensive, as I am strongly
inclined to believe from my examination of the Coral Reefs
of the great oceans — or if, confining our view to South
CHARLES DARWIN
America, the subsiding movements have been coextensive
with those of elevation, by which, within the same period
of existing shells, the shores of Peru, Chile, Tierra del
Fuego, Patagonia, and La Plata have been upraised — then
we can see that at the same time, at far distant points, cir-
cumstances would have been favourable to the formation of
fossiliferous deposits of wide extent and of considerable
thickness; and such deposits, consequently, would have a
good chance of resisting the wear and tear of successive
beach-lines, and of lasting to a future epoch.
May 21st. — I set out in company with Don Jose Edwards
to the silver-mine of Arqueros, and thence up the valley of
Coquimbo. Passing through a mountainous country, we
reached by nightfall the mines belonging to Mr. Edwards.
I enjoyed my night's rest here from a reason which will not
be fully appreciated in England, namely, the absence of
fleas ! The rooms in Coquimbo swarm with them ; but they
will not live here at the height of only three or four thou-
sand feet: it can scarcely be the trifling diminution of tem-
perature, but some other cause which destroys these
troublesome insects at this place. The mines are now in a
bad state, though they formerly yielded about 2000 pounds
in weight of silver a year. It has been said that " a person
with a copper-mine will gain ; with silver he may gain ; but
with gold he is sure to lose." This is not true: all the large
Chilian fortunes have been made by mines of the more
precious metals. A short time since an English physician
returned to England from Copiapo, taking with him the
profits of one share of a silver-mine, which amounted to
about 24,000 pounds sterling. No doubt a copper-mine with
care is a sure game, whereas the other is gambling, or rather
taking a ticket in a lottery. The owners lose great quan-
tities of rich ores; for no precautions can prevent robberies.
I heard of a gentleman laying a bet with another, that one
of his men should rob him before his face. The ore when
brought out of the mine is broken into pieces, and the use-
less stone thrown on one side. A couple of the miners who
were thus employed, pitched, as if by accident, two fragments
away at the same moment, and then cried out for a joke
THE VOYAGE OF THE BEAGLE 367
" Let us see which rolls furthest." The owner, who was
standing by, bet a cigar with his friend on the race. The
miner by this means watched the very point amongst the
rubbish where the stone lay. In the evening he picked it
up and carried it to his master, showing him a rich mass of
silver-ore, and saying, " This was the stone on which you
won a cigar by its rolling so far."
May 23rd. — We descended into the fertile valley of Co-
quimbo, and followed it till we reached an Hacienda belong-
ing to a relation of Don Jose, where we stayed the next day.
I then rode one day's journey further, to see what were
declared to be some petrified shells and beans, which latter
turned out to be small quartz pebbles. We passed through
several small villages; and the valley was beautifully culti-
vated, and the whole scenery very grand. We were here
near the main Cordillera, and the surrounding hills were
lofty. In all parts of northern Chile, fruit trees produce
much more abundantly at a considerable height near the
Andes than in the lower country. The figs and grapes of
this district are famous for their excellence, and are cul-
tivated to a great extent. This valley is, perhaps, the most
productive one north of Quillota. I believe it contains,
including Coquimbo, 25,000 inhabitants. The next day I
returned to the Hacienda, and thence, together with Don
Jose, to Coquimbo.
June 2nd. — We set out for the valley of Guasco, following
the coast-road, which was considered rather less desert than
the other. Our first day's ride was to a solitary house, called
Yerba Buena, where there was pasture for our horses. The
shower mentioned as having fallen, a fortnight ago, only
reached about half-way to Guasco; we had, therefore, in the
first part of our journey a most faint tinge of green, which
soon faded quite away. Even where brightest, it was scarcely
sufficient to remind one of the fresh turf and budding
flowers of the spring of other countries. While travelling
through these deserts one feels like a prisoner shut up in
a gloomy court, who longs to see something green and to
smell a moist atmosphere.
June 3rd. — Yerba Buena to Carizal. During the first part
of the day we crossed a mountainous rocky desert, and after-
368 CHARLES DARWIN
wards a long deep sandy plain, strewed with broken sea-
shells. There was very little water, and that little saline:
the whole country, from the coast to the Cordillera, is an un-
inhabited desert. I saw traces only of one living animal in
abundance, namely, the shells of a Bulimus, which were
collected together in extraordinary numbers on the driest
spots. In the spring one humble little plant sends out a few
leaves, and on these the snails feed. As they are seen only
very early in the morning, when the ground is slightly damp
with dew, the Guascos believe that they are bred from it. I
have observed in other places that extremely dry and sterile
districts, where the soil is calcareous, are extraordinarily
favourable to land-shells. At Carizal there were a few cot-
tages, some brackish water, and a trace of cultivation : but it
was with difficulty that we purchased a little corn and straw
for our horses.
4th. — Carizal to Sauce. We continued to ride over desert
plains, tenanted by large herds of guanaco. We crossed also
the valley of Chaneral ; which, although the most fertile one
between Guasco and Coquimbo, is very narrow, and produces
so little pasture, that we could not purchase any for our
horses. At Sauce we found a very civil old gentleman, super-
intendent of a copper-smelting furnace. As an especial
favour, he allowed me to purchase at a high price an armful
of dirty straw, which was all the poor horses had for supper
after their long day's journey. Few smelting- furnaces are
now at work in any part of Chile ; it is found more profitable,
on account of the extreme scarcity of firewood, and from
the Chilian method of reduction being so unskilful, to ship the
ore for Swansea. The next day we crossed some mountains
to Freyrina, in the valley of Guasco. During each day's ride
further northward, the vegetation became more and more
scanty; even the great chandelier-like cactus was here re-
placed by a different and much smaller species. During the
winter months, both in northern Chile and in Peru, a uniform
bank of clouds hangs, at no great height, over the Pacific.
From the mountains we had a very striking view of this
white and brilliant aerial-field, which sent arms up the valleys,
leaving islands and promontories in the same manner, as the
sea does in the Chonos archipelago and in Tierra del Fuego.
THE VOYAGE OF THE BEAGLE 369
We stayed two days at Freyrina. In the valley of Guasco
there are four small towns. At the mouth there is the port, a
spot entirely desert, and without any water in the immediate
neighbourhood. Five leagues higher up stands Freyrina, a
long straggling village, with decent whitewashed houses.
Again, ten leagues further up Ballenar is situated, and above
this Guasco Alto, a horticultural village, famous for its dried
fruit. On a clear day the view up the valley is very fine ; the
straight opening terminates in the far-distant snowy Cordil-
lera; on each side an infinity of crossing-lines are blended
together in a beautiful haze. The foreground is singular
from the number of parallel and step-formed terraces; and
the included strip of green valley, with its willow-bushes, is
contrasted on both hands with the naked hills. That the sur-
rounding country was most barren will be readily believed,
when it is known that a shower of rain had not fallen during
the last thirteen months. The inhabitants heard with the
greatest envy of the rain at Coquimbo ; from the appearance
of the sky they had hopes of equally good fortune, which, a
fortnight afterwards, were realized. I was at Copiapo at the
time; and there the people, with equal envy, talked of the
abundant rain at Guasco. After two or three very dry years,
perhaps with not more than one shower during the whole
time, a rainy year generally follows ; and this does more harm
than even the drought. The rivers swell, and cover with
gravel and sand the narrow strips of ground, which alone are
fit for cultivation. The floods also injure the irrigating
ditches. Great devastation had thus been caused three years
ago.
June 8th. — We rode on to Ballenar, which takes its name
from Ballenagh in Ireland, the birthplace of the family of
O'Higgins, who, under the Spanish government, were presi-
dents and generals in Chile. As the rocky mountains on each
hand were concealed by clouds, the terrace-like plains gave
to the valley an appearance like that of Santa Cruz in Pata-
gonia. After spending one day at Ballenar I set out, on the
ioth, for the upper part of the valley of Copiapo. We rode
all day over an uninteresting country. I am tired of repeat-
ing the epithets barren and sterile. These words, however,
as commonly used, are comparative; I have always applied
370 CHARLES DARWIN
them to the plains of Patagonia, which can boast of spiny
bushes and some tufts of grass ; and this is absolute fertility,
as compared with northern Chile. Here again, there are not
many spaces of two hundred yards square, where some little
bush, cactus or lichen, may not be discovered by careful
examination; and in the soil seeds lie dormant ready to
spring up during the first rainy winter. In Peru real deserts
occur over wide tracts of country. In the evening we
arrived at a valley, in which the bed of the streamlet was
damp: following it up, we came to tolerably good water.
During the night, the stream, from not being evaporated
and absorbed so quickly, flows a league lower down than
during the day. Sticks were plentiful for firewood, so that
it was a good place to bivouac for us; but for the poor ani-
mals there was not a mouthful to eat.
June nth. — We rode without stopping for twelve hours,
till we reached an old smelting-furnace, where there was
water and firewood ; but our horses again had nothing to eat,
being shut up in an old courtyard. The line of road was
hilly, and the distant views interesting, from the varied
colours of the bare mountains. It was almost a pity to see
the sun shining constantly over so useless a country; such
splendid weather ought to have brightened fields and pretty
gardens. The next day we reached the valley of Copiapo.
I was heartily glad of it; for the whole journey was a con-
tinued source of anxiety; it was most disagreeable to hear,
whilst eating our own suppers, our horses gnawing the posts
to which they were tied, and to have no means of relieving
their hunger. To all appearance, however, the animals
were quite fresh ; and no one could have told that they had
eaten nothing for the last fifty-five hours.
I had a letter of introduction to Mr. Bingley, who received
me very kindly at the Hacienda of Potrero Seco. This
estate is between twenty and thirty miles long, but very nar-
row, being generally only two fields wide, one on each side
the river. In some parts the estate is of no width, that is
to say, the land cannot be irrigated, and therefore is value-
less, like the surrounding rocky desert. The small quantity
of cultivated land in the whole line of valley, does not so
much depend on inequalities of level, and consequent unfit-
THE VOYAGE OF THE BEAGLE 371
ness for irrigation, as on the small supply of water. The
river this year was remarkably full : here, high up the valley,
it reached to the horse's belly, and was about fifteen yards
wide, and rapid; lower down it becomes smaller and smaller,
and is generally quite lost, as happened during one period
of thirty years, so that not a drop entered the sea. The
inhabitants watch a storm over the Cordillera with great
interest; as one good fall of snow provides them with water
for the ensuing year. This is of infinitely more consequence
than rain in the lower country. Rain, as often as it falls,
which is about once in every two or three years, is a great
advantage, because the cattle and mules can for some time
afterwards find a little pasture in the mountains. But with-
out snow on the Andes, desolation extends throughout the
valley. It is on record that three times nearly all the inhab-
itants have been obliged to emigrate to the south. This year
there was plenty of water, and every man irrigated his
ground as much as he chose; but it has frequently been
necessary to post soldiers at the sluices, to see that each
estate took only its proper allowance during so many hours
in the week. The valley is said to contain 12,000 souls, but
its produce is sufficient only for three months in the year;
the rest of the supply being drawn from Valparaiso and the
south. Before the discovery of the famous silver-mines of
Chanuncillo, Copiapo was in a rapid state of decay; but now
it is in a very thriving condition; and the town, which was
completely overthrown by an earthquake, has been rebuilt.
The valley of Copiapo, forming a mere ribbon of green
in a desert, runs in a very southerly direction; so that it is
of considerable length to its source in the Cordillera. The
valleys of Guasco and Copiapo may both be considered as
long narrow islands, separated from the rest of Chile by
deserts of rock instead of by salt water. Northward of
these, there is one other very miserable valley, called Paposo,
which contains about two hundred souls; and then there
extends the real desert of Atacama— a barrier far worse
than the most turbulent ocean. After staying a few days at
Potrero Seco, I proceeded up the valley to the house of Don
Benito Cruz, to whom I had a letter of introduction. I found
him most hospitable; indeed it is impossible to bear too
372 CHARLES DARWIN
strong testimony to the kindness with which travellers are
received in almost every part of South America. The next
day I hired some mules to take me by the ravine of Jol-
quera into the central Cordillera. On the second night the
weather seemed to foretell a storm of snow or rain, and whilst
lying in our beds we felt a trifling shock of an earthquake.
The connection between earthquakes and the weather has
been often disputed : it appears to me to be a point of great
interest, which is little understood. Humboldt has remarked
in one part of the Personal Narrative, 1 that it would be
difficult for any person who had long resided in New Anda-
lusia, or in Lower Peru, to deny that there exists some con-
nection between these phenomena : in another part, however,
he seems to think the connection fanciful. At Guayaquil,
it is said that a heavy shower in the dry season is invariably
followed by an earthquake. In Northern Chile, from the
extreme infrequency of rain, or even of weather foreboding
rain, the probability of accidental coincidences becomes very
small; yet the inhabitants are here most firmly convinced of
some connection between the state of the atmosphere and of
the trembling of the ground: I was much struck by this,
when mentioning to some people at Copiapo that there had
been a sharp shock at Coquimbo : they immediately cried out,
" How fortunate ! there will be plenty of pasture there this
year." To their minds an earthquake foretold rain, as surely
as rain foretold abundant pasture. Certainly it did so hap-
pen that on the very day of the earthquake, that shower of
rain fell, which I have described as in ten days' time pro-
ducing a thin sprinkling of grass. At other times rain has
followed earthquakes at a period of the year when it is a
far greater prodigy than the earthquake itself: this happened
after the shock of November, 1822, and again in 1829, at
Valparaiso; also after that of September, 1833, at Tacna.
A person must be somewhat habituated to the climate of
these countries to perceive the extreme improbability of rain
falling at such seasons, except as a consequence of some law
1 Vol. iv. p. 11, and vol. ii. p. 217. For the remarks on Guayaquil, see
Silliman's Journ., vol. xxiv. p. 384. For those on Tacna by Mr. Hamilton,
see Trans, of British Association, 1840. For those on Coseguina see Mr.
Caldcleugh in Phil. Trans., 1835. In the former edition I collected several
references on the coincidences between sudden falls in the barometer and
earthquakes; and between earthquakes and meteors.
THE VOYAGE OF THE BEAGLE 373
quite unconnected with the ordinary course of the weather.
In the cases of great volcanic eruptions, as that of Co-
seguina, where torrents of rain fell at a time of the year most
unusual for it, and "almost unprecedented in Central
America," it is not difficult to understand that the volumes
of vapour and clouds of ashes might have disturbed the
atmospheric equilibrium. Humboldt extends this view to
the case of earthquakes unaccompanied by eruptions; but I
can hardly conceive it possible, that the small quantity of
aeriform fluids which then escape from the fissured ground,
can produce such remarkable effects. There appears much
probability in the view first proposed by Mr. P. Scrope, that
when the barometer is low, and when rain might naturally
be expected to fall, the diminished pressure of the atmos-
phere over a wide extent of country, might well determine
the precise day on which the earth, already stretched to the
utmost by the subterranean forces, should yield, crack, and
consequently tremble. It is, however, doubtful how far this
idea will explain the circumstances of torrents of rain fall-
ing in the dry season during several days, after an earth-
quake unaccompanied by an eruption; such cases seem to
bespeak some more intimate connection between the atmos-
pheric and subterranean regions.
Finding little of interest in this part of the ravine, we
retraced our steps to the house of Don Benito, where I stayed
two days collecting fossil shells and wood. Great prostrate
silicified trunks of trees, embedded in a conglomerate, were
extraordinarily numerous. I measured one, which was fif-
teen feet in circumference: how surprising it is that every
atom of the woody matter in this great cylinder should have
been removed and replaced by silex so perfectly, that each
vessel and pore is preserved ! These trees flourished at about
the period of our lower chalk; they all belonged to the fir-
tribe. It was amusing to hear the inhabitants discussing the
nature of the fossil shells which I collected, almost in the
same terms as were used a century ago in Europe, — namely,
whether or not they had been thus " born by nature." My
geological examination of the country generally created a
good deal of surprise amongst the Chilenos: it was long
before they could be convinced that I was not hunting for
374 CHARLES DARWIN
mines. This was sometimes troublesome: I found the most
ready way of explaining my employment, was to ask them
how it was that they themselves were not curious concerning
earthquakes and volcanos? — why some springs were hot and
others cold? — why there were mountains in Chile, and not
a hill in La Plata? These bare questions at once satisfied
and silenced the greater number; some, however (like a few
in England who are a century behindhand), thought that all
such inquiries were useless and impious; and that it was
quite sufficient that God had thus made the mountains.
An order had recently been issued that all stray dogs
should be killed, and we saw many lying dead on the road. A
great number had lately gone mad, and several men had been
bitten and had died in consequence. On several occasions
hydrophobia has prevailed in this valley. It is remarkable
thus to find so strange and dreadful a disease, appearing
time after time in the same isolated spot. It has been
remarked that certain villages in England are in like manner
much more subject to this visitation than others. Dr. Una-
nue states that hydrophobia was first known in South
America in 1803: this statement is corroborated by Azara
and Ulloa having never heard of it in their time. Dr. Una-
nue says that it broke out in Central America, and slowly
travelled southward. It reached Arequipa in 1807 ; and it is
said that some men there, who had not been bitten, were
affected, as were some negroes, who had eaten a bullock
which had died of hydrophobia. At lea forty-two people thus
miserably perished. The disease came on between twelve
and ninety days after the bite; and in those cases where it
did come on, death ensued invariably within five days. After
1808, a long interval ensued without any cases. On inquiry,
I did not hear of hydrophobia in Van Diemen's Land, or in
Australia; and Burchell says, that during the five years he
was at the Cape of Good Hope, he never heard of an instance
of it. Webster asserts that at the Azores hydrophobia has
never occurred; and the same assertion has been made with
respect to Mauritius and St. Helena. 2 In so strange a disease
2 Observa. sobre el Clima de Lima, p. 67. — Azara's Travels, vol. i. p. 381.
— Ulloa's Voyage, vol. ii. p. 28. — Burchell's Travels, vol. ii. p. 524. — Web-
ster's Description of the Azores, p. 124. — Voyage a l'Isle de France par un
Officier du Koi, torn. i. p. 248. — Description of St. Helena, p. 123.
THE VOYAGE OF THE BEAGLE 375
some information might possibly be gained by considering
the circumstances under which it originates in distant cli-
mates ; for it is improbable that a dog already bitten, should
have been brought to these distant countries.
At night, a stranger arrived at the house of Don Benito,
and asked permission to sleep there. He said he had been
wandering about the mountains for seventeen days, having
lost his way. He started from Guasco, and being accustomed
to travelling in the Cordillera, did not expect any difficulty
in following the track to Copiapo; but he soon became
involved in a labyrinth of mountains, whence he could not
escape. Some of his mules had fallen over precipices, and he
had been in great distress. His chief difficulty arose from
not knowing where to find water in the lower country, so that
he was obliged to keep bordering the central ranges.
We returned down the valley, and on the 22nd reached
the town of Copiapo. The lower part of the valley is broad,
forming a fine plain like that of Quillota. The town covers
a considerable space of ground, each house possessing a gar-
den : but it is an uncomfortable place, and the dwellings are
poorly furnished. Every one seems bent on the one object
of making money, and then migrating as quickly as possible.
All the inhabitants -are more or less directly concerned with
mines; and mines and ores are the sole subjects of conver-
sation. Necessaries of all sorts are extremely dear; as the
distance from the town to the port is eighteen leagues, and
the land carriage very expensive. A fowl costs five or six
shillings; meat is nearly as dear as in England; firewood,
or rather sticks, are brought on donkeys from a distance of
two and three days' journey within the Cordillera; and pas-
turage for animals is a shilling a day: all this for South
America is wonderfully exorbitant.
June 26th. — I hired a guide and eight mules to take me
into the Cordillera by a different line from my last excur-
sion. As the country was utterly desert, we took a cargo
and a half of barley mixed with chopped straw. About two
leagues above the town a broad valley called the " Despo-
blado," or uninhabited, branches off from that one by which
we had arrived. Although a valley of the grandest dimen-
376 CHARLES DARWIN
sions, and leading to a pass across the Cordillera, yet it is
completely dry, excepting perhaps for a few days during
some very rainy winter. The sides of the crumbling moun-
tains were furrowed by scarcely any ravines ; and the bottom
of the main valley, filled with shingle, was smooth and nearly
level. No considerable torrent could ever have flowed down
this bed of shingle; for if it had, a great cliff -bounded chan-
nel, as in all the southern valleys, would assuredly have been
formed. I feel little doubt that this valley, as well as those
mentioned by travellers in Peru, were left in the state we now
see them by the waves of the sea, as the land slowly rose. I
observed in one place, where the Despoblado was joined by a
ravine (which in almost any other chain would have been
called a grand valley), that its bed, though composed merely
of sand and gravel, was higher than that of its tributary.
A mere rivulet of water, in the course of an hour, would have
cut a channel for itself; but it was evident that ages had
passed away, and no such rivulet had drained this great tribu-
tary. It was curious to behold the machinery, if such a term
may be used, for the drainage, all, with the last trifling excep-
tion, perfect, yet without any signs of action. Every one
must have remarked how mud-banks, left by the retiring tide,
imitate in miniature a country with hill and dale; and here
we have the original model in rock, formed as the continent
rose during the secular retirement of the ocean, instead of
during the ebbing and flowing of the tides. If a shower of
rain falls on the mud-bank, when left dry, it deepens the
already- formed shallow lines of excavation ; and so it is with
the rain of successive centuries on the bank of rock and soil,
which we call a continent.
We rode on after it was dark, till we reached a side ravine
with a small well, called " Agua amarga." The water
deserved its name, for besides being saline it was most offen-
sively putrid and bitter ; so that we could not force ourselves
to drink either tea or mate. I suppose the distance from the
river of Copiapo to this spot was at least twenty-five or thirty
English miles; in the whole space there was not a single
drop of water, the country deserving the name of desert in
the strictest sense. Yet about half way we passed some old
Indian ruins near Punta Gorda: I noticed also in front of
THE VOYAGE OF THE BEAGLE 377
some of the valleys, which branch off from the Despoblado,
two piles of stones placed a little way apart, and directed so
as to point up the mouths of these small valleys. My com-
panions knew nothing about them, and only answered my
queries by their imperturbable " quien sabe ? "
I observed Indian ruins in several parts of the Cordillera :
the most perfect which I saw, were the Ruinas de Tambillos,
in the Uspallata Pass. Small square rooms were there hud-
dled together in separate groups : some of the doorways were
yet standing; they were formed by a cross slab of stone only
about three feet high. Ulloa has remarked on the lowness of
the doors in the ancient Peruvian dwellings. These houses,
when perfect, must have been capable of containing a con-
siderable number of persons. Tradition says, that they were
used as halting-places for the Incas, when they crossed the
mountains. Traces of Indian habitations have been dis-
covered in many other parts, where it does not appear proba-
ble that they were used as mere resting-places, but yet where
the land is as utterly unfit for any kind of cultivation, as it is
near the Tambillos or at the Incas Bridge, or in the Portillo
Pass, at all which places I saw ruins. In the ravine of
Jajuel, near Aconcagua, where there is no pass, I heard of
remains of houses situated at a great height, where it is
extremely cold and sterile. At first I imagined that these
buildings had been places of refuge, built by the Indians on
the first arrival of the Spaniards; but I have since been
inclined to speculate on the probability of a small change of
climate.
In this northern part of Chile, within the Cordillera, old
Indian houses are said to be especially numerous : by digging
amongst the ruins, bits of woollen articles, instruments of
precious metals, and heads of Indian corn, are not unfre-
quently discovered: an arrow-head made of agate, and of
precisely the same form with those now used in Tierra del
Fuego, was given me. I am aware that the Peruvian Indians
now frequently inhabit most lofty and bleak situations; but
at Copiapo I was assured by men who had spent their lives in
travelling through the Andes, that there were very many
(muchisimas) buildings at heights so great as almost to bor-
der upon the perpetual snow, and in parts where there exist
378 CHARLES DARWIN
no passes, and where the land produces absolutely nothing,
and what is still more extraordinary, where there is no water.
Nevertheless it is the opinion of the people of the country
(although they are much puzzled by the circumstance), that,
from the appearance of the houses, the Indians must have
used them as places of residence. In this valley, at Punta
Gorda, the remains consisted of seven or eight square little
rooms, which were of a similar form with those at Tambillos,
but built chiefly of mud, which the present inhabitants can-
not, either here or, according to Ulloa, in Peru, imitate in
durability. They were situated in the most conspicuous and
defenceless position, at the bottom of the flat broad valley.
There was no water nearer than three or four leagues, and
that only in very small quantity, and bad : the soil was abso-
lutely sterile ; I looked in vain even for a lichen adhering to
the rocks. At the present day, with the advantage of beasts
of burden, a mine, unless it were very rich, could scarcely
be worked here with profit. Yet the Indians formerly chose
it as a place of residence! If at the present time two or
three showers of rain were to fall annually, instead of one,
as now is the case during as many years, a small rill of water
would probably be formed in this great valley; and then, by
irrigation (which was formerly so well understood by the
Indians), the soil would easily be rendered sufficiently pro-
ductive to support a few families.
I have convincing proofs that this part of the continent of
South America has been elevated near the coast at least from
400 to 500, and in some parts from 1000 to 1300 feet, since
the epoch of existing shells; and further inland the rise pos-
sibly may have been greater. As the peculiarly arid character
of the climate is evidently a consequence of the height of the
Cordillera, we may feel almost sure that before the later ele-
vations, the atmosphere could not have been so completely
drained of its moisture as it now is ; and as the rise has been
gradual, so would have been the change in climate. On this
notion of a change of climate since the buildings were
inhabited, the ruins must be of extreme antiquity, but I do
not think their preservation under the Chilian climate any
great difficulty. We must also admit on this notion (and
this perhaps is a greater difficulty) that man has inhabited
THE VOYAGE OF THE BEAGLE 379
South America for an immensely long period, inasmuch as
any change of climate effected by the elevation of the land
must have been extremely gradual. At Valparaiso, within
the last 220 years, the rise has been somewhat less than 19
feet : at Lima a sea-beach has certainly been upheaved from
80 to 90 feet, within the Indo-human period: but such small
elevations could have had little power in deflecting the mois-
ture-bringing atmospheric currents. Dr. Lund, however,
found human skeletons in the caves of Brazil, the appearance
of which induced him to believe that the Indian race has
existed during a vast lapse of time in South America.
When at Lima, I conversed on these subjects 8 with Mr.
Gill, a civil engineer, who had seen much of the interior
country. He told me that a conjecture of a change of cli-
mate had sometimes crossed his mind; but that he thought
that the greater portion of land, now incapable of cultivation,
but covered with Indian ruins, had been reduced to this state
by the water-conduits, which the Indians formerly con-
structed on so wonderful a scale, having been injured by
neglect and by subterranean movements. I may here men-
tion, that the Peruvians actually carried their irrigating
streams in tunnels through hills of solid rock. Mr. Gill told
me, he had been employed professionally to examine one:
he found the passage low, narrow, crooked, and not of uni-
form breadth, but of very considerable length. Is it not
most wonderful that men should have attempted such opera-
tions, without the use of iron or gunpowder? Mr. Gill also
mentioned to me a most interesting, and, as far as I am
aware, quite unparalleled case, of a subterranean disturbance
having changed the drainage of a country. Travelling from
Casma to Huaraz (not very far distant from Lima), he
found a plain covered with ruins and marks of ancient culti-
vation, but now quite barren. Near it was the dry course of
a considerable river, whence the water for irrigation had for-
merly been conducted. There was nothing in the appearance
of the water-course to indicate that the river had not flowed
8 Temple, in his travels through Upper Peru, or Bolivia, in going from
Potosi to Oruro, says, " I saw many Indian villages or dwellings in ruins,
up even to the very tops of the mountains, attesting a former population
where now all is desolate." He makes similar remarks in anotner place;
but I cannot tell whether this desolation has been caused by a want of
population, or by an altered condition of the land.
380 CHARLES DARWIN
there a few years previously ; in some parts, beds of sand and
gravel were spread out; in others, the solid rock had been
worn into a broad channel, which in one spot was about 40
yards in breadth and 8 feet deep. It is self-evident that a
person following up the course of a stream, will always
ascend at a greater or less inclination: Mr. Gill, therefore,
was much astonished, when walking up the bed of this
ancient river, to find himself suddenly going down hill. He
imagined that the downward slope had a fall of about 40 or
50 feet perpendicular. We here have unequivocal evidence
that a ridge had been uplifted right across the old bed of a
stream. From the moment the river-course was thus arched,
the water must necessarily have been thrown back, and a new
channel formed. From that moment, also, the neighbouring
plain must have lost its fertilizing stream, and become a
desert.
June 27th. — We set out early in the morning, and by mid-
day reached the ravine of Paypote, where there is a tiny rill
of water, with a little vegetation, and even a few algarroba
trees, a kind of mimosa. From having fire-wood, a smelting-
furnace had formerly been built here: we found a solitary
man in charge of it, whose sole employment was hunting
guanacos. At night it froze sharply ; but having plenty of
wood for our fire, we kept ourselves warm.
28th. — We continued gradually ascending, and the valley
now changed into a ravine. During the day we saw several
guanacos, and the track of the closely-allied species, the
Vicuna: this latter animal is pre-eminently alpine in its
habits ; it seldom descends much below the limit of perpetual
snow, and therefore haunts even a more lofty and sterile
situation than the guanaco. The only other animal which we
saw in any number was a small fox: I suppose this animal
preys on the mice and other small rodents, which, as long as
there is the least vegetation, subsist in considerable numbers
in very desert places. In Patagonia, even on the borders of
the salinas, where a drop of fresh water can never be found,
excepting dew, these little animals swarm. Next to lizards,
mice appear to be able to support existence on the smallest
and driest portions of the earth — even on islets in the midst
of great oceans.
THE VOYAGE OF THE BEAGLE 381
The scene on all sides showed desolation, brightened and
made palpable by a clear, unclouded sky. For a time such
scenery is sublime, but this feeling cannot last, and then it
becomes uninteresting. We bivouacked at the foot of the
" primera linea," or the first line of the partition of waters.
The streams, however, on the east side do not flow to the
Atlantic, but into an elevated district, in the middle of which
there is a large saline, or salt lake ; thus forming a little Cas-
pian Sea at the height, perhaps, of ten thousand feet. Where
we slept, there were some considerable patches of snow, but
they do not remain throughout the year. The winds in these
lofty regions obey very regular laws: every day a fresh
breeze blows up the valley, and at night, an hour or two after
sunset, the air from the cold regions above descends as
through a funnel. This night it blew a gale of wind, and the
temperature must have been considerably below the freezing-
point, for water in a vessel soon became a block of ice. No
clothes seemed to oppose any obstacle to the air; I suffered
very much from the cold, so that I could not sleep, and in
the morning rose with my body quite dull and benumbed.
In the Cordillera further southward, people lose their lives
from snowstorms; here, it sometimes happens from another
cause. My guide, when a boy of fourteen years old, was
passing the Cordillera with a party in the month of May;
and while in the central parts, a furious gale of wind arose,
so that the men could hardly cling on their mules, and stones
were flying along the ground. The day was cloudless, and
not a speck of snow fell, but the temperature was low. It is
probable that the thermometer could not have stood very
many degrees below the freezing-point, but the effect on
their bodies, ill protected by clothing, must have been in pro-
portion to the rapidity of the current of cold air. The gale
lasted for more than a day; the men began to lose their
strength, and the mules would not move onwards. My guide's
brother tried to return, but he perished, and his body was
found two years afterwards, lying by the side of his mule
near the road, with the bridle still in his hand. Two other
men in the party lost their fingers and toes ; and out of two
hundred mules and thirty cows, only fourteen mules escaped
alive. Many years ago the whole of a large party are sup-
382 CHARLES DARWIN
posed to have perished from a similar cause, but their bodies
to this day have never been discovered. The union of a
cloudless sky, low temperature, and a furious gale of wind,
must be, I should think, in all parts of the world an unusual
occurrence.
June 2pth. — We gladly travelled down the valley to our
former night's lodging, and thence to near the Agua amarga.
On July ist we reached the valley of Copiapo. The smell of
the fresh clover was quite delightful, after the scentless air
of the dry, sterile Despoblado. Whilst staying in the town I
heard an account from several of the inhabitants, of a hill
in the neighbourhood which they called " El Bramador," — the
roarer or bellower. I did not at the time pay sufficient atten-
tion to the account; but, as far as I understood, the hill was
covered by sand, and the noise was produced only when
people, by ascending it, put the sand in motion. The same
circumstances are described in detail on the authority of
Seetzen and Ehrenberg, 4 as the cause of the sounds which
have been heard by many travellers on Mount Sinai near the
Red Sea. One person with whom I conversed had himself
heard the noise: he described it as very surprising; and he
distinctly stated that, although he could not understand how
it was caused, yet it was necessary to set the sand rolling
down the acclivity. A horse walking over dry coarse sand,
causes a peculiar chirping noise from the friction of the par-
ticles; a circumstance which I several times noticed on the
coast of Brazil.
Three days afterwards I heard of the Beagle's arrival at
the Port, distant eighteen leagues from the town. There is
very little land cultivated down the valley; its wide expanse
supports a wretched wiry grass, which even the donkeys can
hardly eat. This poorness of the vegetation is owing to the
quantity of saline matter with which the soil is impregnated.
The Port consists of an assemblage of miserable little hovels,
situated at the foot of a sterile plain. At present, as the
river contains water enough to reach the sea, the inhabitants
enjoy the advantage of having fresh water within a mile and
a half. On the beach there were large piles of merchandise,
♦Edinburgh Phil. Journ., Jan., 1830, p. 74; and April, 1830, p. 258 — also
Daubeny on Volcanoes, p. 438; and Bengal Journ., vol. vii. p. 324.
THE VOYAGE OF THE BEAGLE 383
and the little place had an air of activity. In the evening
I gave my adios, with a hearty good-will, to my companion
Mariano Gonzales, with whom I had ridden so many leagues
in Chile. The next morning the Beagle sailed for Iquique.
July 12th. — We anchored in the port of Iquique, in lat.
20° 12', on the coast of Peru. The town contains about a
thousand inhabitants, and stands on a little plain of sand at
the foot of a great wall of rock, 2000 feet in height, here
forming the coast. The whole is utterly desert. A light
shower of rain falls only once in very many years; and the
ravines consequently are filled with detritus, and the moun-
tain-sides covered by piles of fine white sand, even to a height
of a thousand feet. During this season of the year a heavy
bank of clouds, stretched over the ocean, seldom rises above
the wall of rocks on the coast. The aspect of the place was
most gloomy; the little port, with its few vessels, and small
group of wretched houses, seemed overwhelmed and out of
all proportion with the rest of the scene.
The inhabitants live like persons on board a ship: every
necessary comes from a distance : water is brought in boats
from Pisagua, about forty miles northward, and is sold at
the rate of nine reals (4s. 6d.) an eighteen-gallon cask: I
bought a wine-bottle full for threepence. In like manner
firewood, and of course every article of food, is imported.
Very few animals can be maintained in such a place : on the
ensuing morning I hired with difficulty, at the price of four
pounds sterling, two mules and a guide to take me to the
nitrate of soda works. These are at present the support of
Iquique. This salt was first exported in 1830: in one year an
amount in value of one hundred thousand pounds sterling,
was sent to France and England. It is principally used as a
manure and in the manufacture of nitric acid: owing to its
deliquescent property it will not serve for gunpowder. For-
merly there were two exceedingly rich silver-mines in this
neighbourhood, but their produce is now very small.
Our arrival in the offing caused some little apprehension.
Peru was in a state of anarchy; and each party having
demanded a contribution, the poor town of Iquique was in
tribulation, thinking the evil hour was come. The people
had also their domestic troubles; a short time before, three
384 CHARLES DARWIN
French carpenters had broken open, during the same night,
the two churches, and stolen all the plate : one of the robbers,
however, subsequently confessed, and the plate was recovered.
The convicts were sent to Arequipa, which though the capital
of this province, is two hundred leagues distant ; the govern-
ment there thought it a pity to punish such useful workmen,
who could make all sorts of furniture; and accordingly
liberated them. Things being in this state, the churches were
again broken open, but this time the plate was not recovered.
The inhabitants became dreadfully enraged, and declaring
that none but heretics would thus " eat God Almighty," pro-
ceeded to torture some Englishmen, with the intention of
afterwards shooting them. At last the authorities interfered,
and peace was established.
13th. — In the morning I started for the saltpetre-works,
a distance of fourteen leagues. Having ascended the steep
coast-mountains by a zigzag sandy track, we soon came in
view of the mines of Guantajaya and St. Rosa. These two
small villages are placed at the very mouths of the mines;
and being perched up on hills, they had a still more unnatural
and desolate appearance than the town of Iquique. We did
not reach the saltpetre-works till after sunset, having ridden
all day across an undulating country, a complete and utter
desert. The road was strewed with the bones and dried skins
of many beasts of burden which had perished on it from
fatigue. Excepting the Vultur aura, which preys on the
carcasses, I saw neither bird, quadruped, reptile, nor insect.
On the coast-mountains, at the height of about 2000 feet,
where during this season the clouds generally hang, a very
few cacti were growing in the clefts of rock; and the loose
sand was strewed over with a lichen, which lies on the sur-
face quite unattached. This plant belongs to the genus
Cladonia, and somewhat resembles the reindeer lichen. In
some parts it was in sufficient quantity to tinge the sand,
as seen from a distance, of a pale yellowish colour. Further
inland, during the whole ride of fourteen leagues, I saw only
one other vegetable production, and that was a most minute
yellow lichen, growing on the bones of the dead mules. This
was the first true desert which I had seen: the effect on me
THE VOYAGE OF THE BEAGLE 385
was not impressive; but I believe this was owing to my
having become gradually accustomed to such scenes, as I
rode northward from Valparaiso, through Coquimbo, to Co-
piapo. The appearance of the country was remarkable, from
being covered by a thick crust of common salt, and of a strat-
ified saliferous alluvium, which seems to have been deposited
as the land slowly rose above the level of the sea. The salt
is white, very hard, and compact: it occurs in water- worn
nodules projecting from the agglutinated sand, and is asso-
ciated with much gypsum. The appearance of this super-
ficial mass very closely resembled that of a country after
snow, before the last dirty patches are thawed. The existence
of this crust of a soluble substance over the whole face of
the country, shows how extraordinarily dry the climate must
have been for a long period.
At night I slept at the house of the owner of one of the
saltpetre mines. The country is here as unproductive as
near the coast ; but water, having rather a bitter and brackish
taste, can be procured by digging wells. The well at this
house was thirty-six yards deep : as scarcely any rain falls,
it is evident the water is not thus derived; indeed if it were,
it could not fail to be as salt as brine, for the whole sur-
rounding country is incrusted with various saline substances.
We must therefore conclude that it percolates under ground
from the Cordillera, though distant many leagues. In that
direction there are a few small villages, where the inhabit-
ants, having more water, are enabled to irrigate a little land,
and raise hay, on which the mules and asses, employed in
carrying the saltpetre, are fed. The nitrate of soda was now
selling at the ship's side at fourteen shillings per hundred
pounds: the chief expense is its transport to the sea-coast.
The mine consists of a hard stratum, between two and three
feet thick, of the nitrate mingled with a little of the sulphate
of soda and a good deal of common salt. It lies close beneath
the surface, and follows for a length of one hundred and
fifty miles the margin of a grand basin or plain; this, from
its outline, manifestly must once have been a lake, or more
probably an inland arm of the sea, as may be inferred from
the presence of iodic salts in the saline stratum. The surface
of the plain is. 33 bo feet above the Pacific.
VOL. XXIX— m hc
386 CHARLES DARWIN
ipth. — We anchored in the Bay of Callao, the seaport of
Lima, the capital of Peru. We stayed here six weeks, but
from the troubled state of public affairs, I saw very little of
the country. During our whole visit the climate was far
from being so delightful, as it is generally represented. A
dull heavy bank of clouds constantly hung over the land, so
that during the first sixteen days I had only one view of the
Cordillera behind Lima. These mountains, seen in stages,
one above the other, through openings in the clouds, had a
very grand appearance. It is almost become a proverb, that
rain never falls in the lower part of Peru. Yet this can
hardly be considered correct ; for during almost every day of
our visit there was a thick drizzling mist, which was sufficient
to make the streets muddy and one's clothes damp: this the
people are pleased to call Peruvian dew. That much rain
does not fall is very certain, for the houses are covered only
with flat roofs made of hardened mud; and on the mole ship-
loads of wheat were piled up, being thus left for weeks to-
gether without any shelter.
I cannot say I liked the very little I saw of Peru: in
summer, however, it is said that the climate is much pleas-
anter. In all seasons, both inhabitants and foreigners suffer
from severe attacks of ague. This disease is common on the
whole coast of Peru, but is unknown in the interior. The
attacks of illness which arise from miasma never fail to ap-
pear most mysterious. So difficult is it to judge from the
aspect of a country, whether or not it is healthy, that if a
person had been told to choose within the tropics a situation
appearing favourable for health, very probably he would
have named this coast. The plain round the outskirts of
Callao is sparingly covered with a coarse grass, and in some
parts there are a few stagnant, though very small, pools of
water. The miasma, in all probability, arises from these:
for the town of Arica was similarly circumstanced, and its
healthiness was much improved by the drainage of some
little pools. Miasma is not always produced by a luxuriant
vegetation with an ardent climate; for many parts of Bra-
zil, even where there are marshes and a rank vegetation, are
much more healthy than this sterile coast of Peru. The
densest forests in a temperate climate, as in Chiloe, do not
THE VOYAGE OF THE BEAGLE 387
seem in the slightest degree to affect the healthy condition
of the atmosphere.
The island of St. Jago, at the Cape de Verds, offers an-
other strongly marked instance of a country, which any one
would have expected to find most healthy, being very much
the contrary. I have described the bare and open plains as
supporting, during a few weeks after the rainy season, a thin
vegetation, which directly withers away and dries up : at this
period the air appears to become quite poisonous; both na-
tives and foreigners often being affected with violent fevers.
On the other hand, the Galapagos Archipelago, in the Pa-
cific, with a similar soil, and periodically subject to the same
process of vegetation, is perfectly healthy. Humboldt has
observed, that, " under the torrid zone, the smallest marshes
are the most dangerous, being surrounded, as at Vera Cruz
and Carthagena, with an arid and sandy soil, which raises
the temperature of the ambient air." 5 On the coast of Peru,
however, the temperature is not hot to any excessive degree ;
and perhaps in consequence, the intermittent fevers are not
of the most malignant order. In all unhealthy countries the
greatest risk is run by sleeping on shore. Is this owing to
the state of the body during sleep, or to a greater abundance
of miasma at such times? It appears certain that those
who stay on board a vessel, though anchored at only a short
distance from the coast, generally suffer less than those
actually on shore. On the other hand, I have heard of one
remarkable case where a fever broke out among the crew of
a man-of-war some hundred miles off the coast of Africa,
and at the same time one of those fearful periods* of death
commenced at Sierra Leone.
No state in South America, since the declaration of inde-
pendence, has suffered more from anarchy than Peru. At
the time of our visit, there were four chiefs in arms con-
tending for supremacy in the government: if one succeeded
in becoming for a time very powerful, the others coalesced
against him; but no sooner were they victorious, than they
■Political Essay on the Kingdom of New Spain, vol. iv. p. iqq-.
6 A similar interesting case is recorded in the Madras Medical Quart.
Journ., 1839, p. 340. Dr. Ferguson, in his admirable Paper (see 9th vol. of
Edinburgh Royal Trans.), shows clearly that the poison is generated in
the drying process; and hence that dry hot countries are often *he most
unhealthy.
388 CHARLES DARWIN
were again hostile to each other. The other day, at the An-
niversary of the Independence, high mass was performed, the
President partaking of the sacrament: during the Te Deum
laudamus, instead of each regiment displaying the Peruvian
flag, a black one with death's head was unfurled. Imagine
a government under which such a scene could be ordered, on
such an occasion, to be typical of their determination of
fighting to death ! This state of affairs happened at a time
very unfortunately for me, as I was precluded from taking
any excursions much beyond the limits of the town. The
barren island of St. Lorenzo, which forms the harbour, was
nearly the only place where one could walk securely. The
upper part, which is upwards of iooo feet in height, during
this season of the year (winter), comes within the lower
limit of the clouds; and in consequence, an abundant crypto-
gamic vegetation, and a few flowers cover the summit. On
the hills near Lima, at a height but little greater, the ground
is carpeted with moss, and beds of beautiful yellow lilies,
called Amancaes. This indicates a very much greater de-
gree of humidity, than at a corresponding height at Iquique.
Proceeding northward of Lima, the climate becomes damper,
till on the banks of the Guayaquil, nearly under the equator,
we find the most luxuriant forests. The change, however,
from the sterile coast of Peru to that fertile land is described
as taking place rather abruptly in the latitude of Cape Blan-
co, two degrees south of Guayaquil.
Callao is a filthy, ill-built, small seaport. The inhabitants,
both here and at Lima, present every imaginable shade of
mixture, between European, Negro, and Indian blood. They
appear a depraved, drunken set of people. The atmosphere
is loaded with foul smells, and that peculiar one, which may
be perceived in almost every town within the tropics, was
here very strong. The fortress, which withstood Lord Coch-
rane's long siege, has an imposing appearance. But the
President, during our stay, sold the brass guns, and pro-
ceeded to dismantle parts of it. The reason assigned was,
that he had not an officer to whom he could trust so im-
portant a charge. He himself had good reason for thinking
so, as he had obtained the presidentship by rebelling while
in charge of this same fortress. After we left South Amer-
THE VOYAGE OF THE BEAGLE 389
ica, he paid the penalty in the usual manner, by being con-
quered, taken prisoner, and shot.
Lima stands on a plain in a valley, formed during the
gradual retreat of the sea. It is seven miles from Callao,
and is elevated 500 feet above it; but from the slope being
very gradual, the road appears absolutely level ; so that when
at Lima it is difficult to believe one has ascended even one
hundrea feet : Humboldt has remarked on this singularly de-
ceptive case. Steep, barren hills rise like islands from the
plain, which is divided, by straight mud-walls, into large
green fields. In these scarcely a tree grows excepting a few
willows, and an occasional clump of bananas and of oranges.
The city of Lima is now in a wretched state of decay: the
streets are nearly unpaved; and heaps of filth are piled up
in all directions, where the black gallinazos, tame as poultry,
pick up bits of carrion. The houses have generally an upper
story, built jn account of the earthquakes, of plastered wood-
work ; but some of the old ones, which are now used by sev-
eral families, are immensely large, and would rival in suites
of apartments the most magnificent in any place. Lima, the
City of the Kings, must formerly have been a splendid town.
The extraordinary number of churches gives it, even at the
present day, a; peculiar and striking character, especially
when viewed from a short distance.
One day I went out with some merchants to hunt in the
immediate vicinity of the city. Our sport was very poor;
but I had an opportunity of seeing the ruins of one of the
ancient Indian villages, with its mound like a natural hill in
the centre. The remains of houses, enclosures, irrigating
streams, and burial mounds, scattered over this plain, cannot
fail to give one a high idea of the condition and number of
the ancient population. When their earthenware, woollen
clothes, utensils of elegant forms cut out of the hardest rocks,
tools of copper, ornaments of precious stones, palaces, and
hydraulic works, are considered, it is impossible not to re-
spect the considerable advance made by them in the arts of
civilization. The burial mounds, called Huacas, are really
stupendous; although in some places they appear to be nat-
ural hills incased and modelled.
There is also another and very different class of ruins,
390 CHARLES DARWIN
which possesses some interest, namely, those of old Callao,
overwhelmed by the great earthquake of 1746, and its ac-
companying wave. The destruction must have been more
complete even than at Talcahuano. Quantities of shingle
almost conceal the foundations of the walls, and vast masses
of brickwork appear to have been whirled about like pebbles
by the retiring waves. It has been stated that the land sub"
sided during this memorable shock: I could not discover any
proof of this; yet it seems far from improbable, for the
form of the coast must certainly have undergone some change
since the foundation of the old town; as no people in their
senses would willingly have chosen for their building place,
the narrow spit of shingle on which the ruins now stand.
Since our voyage, M. Tschudi has come to the conclusion,
by the comparison of old and modern maps, that the coast
both north and south of Lima has certainly subsided.
On the island of San Lorenzo, there are very satisfactory
proofs of elevation within the recent period; this of course
is not opposed to the belief, of a small sinking of the ground
having subsequently taken place. The side of this island
fronting the Bay of Callao, is worn into three obscure ter-
races, the lower one of which is covered by a bed a mile in
length, almost wholly composed of shells of eighteen species,
now living in the adjoining sea. The height of this bed is
eighty-five feet. Many of the shells are deeply corroded, and
have a much older and more decayed appearance than those
at the height of 500 or 600 feet on the coast of Chile. These
shells are associated with much common salt, a little sul-
phate of lime (both probably left by the evaporation of the
spray, as the land slowly rose), together with sulphate of
soda and muriate of lime. They rest on fragments of the
underlying sandstone, and are covered by a few inches thick
of detritus. The shells, higher up on this terrace, could be
traced scaling off in flakes, and falling into an impalpable
powder; and on an upper terrace, at the height of 170 feet,
and likewise at some considerably higher points, I found a
layer of saline powder of exactly similar appearance, and
lying in the same relative position. I have no doubt that this
upper layer originally existed as a bed of shells, like that on
the eighty-five-feet ledge ; but it does not now contain even a
THE VOYAGE OF THE BEAGLE 391
trace of organic structure. The powder has been analyzed
for me by Mr. T. Reeks; it consists of sulphates and muri-
ates both of lime and soda, with very little carbonate of
lime. It is known that common salt and carbonate of lime
left in a mass for some time together, partly decompose each
other; though this does not happen with small quantities in
solution. As the half-decomposed shells in the lower parts
are associated with much common salt, together with some
of the saline substances composing the upper saline layer,
and as these shells are corroded and decayed in a remarkable
manner, I strongly suspect that this double decomposition
has here taken place. The resultant salts, however, ought
to be carbonate of soda and muriate of lime; the latter is
present, but not the carbonate of soda. Hence I am led to
imagine that by some unexplained means, the carbonate of
soda becomes changed into the sulphate. It is obvious that
the saline layer could not have been preserved in any coun-
try in which abundant rain occasionally fell: on the other
hand, this very circumstance, which at first sight appears so
highly favourable to the long preservation of exposed shells,
has probably been the indirect means, through the common
salt not having been washed away, of their decomposition
and early decay.
I was much interested by finding on the terrace, at the
height of eighty-five feet, embedded amidst the shells and
much sea-drifted rubbish, some bits of cotton thread, plaited
rush, and the head of a stalk of Indian corn: I compared
these relics with similar ones taken out of the Huacas, or old
Peruvian tombs, and found them identical in appearance.
On the mainland in front of San Lorenzo, near Bellavista,
there is an extensive and level plain about a hundred feet
high, of which the lower part is formed of alternating layers
of sand and impure clay, together with some gravel, and the
surface, to the depth of from three to six feet, of a reddish
loam, containing a few scattered sea-shells and numerous
small fragments of coarse red earthenware, more abundant
at certain spots than at others. At first I was inclined to
believe that th!j superficial bed, from its wide extent and
smoothness, must have been deposited beneath the sea; but
I afterwards found in one spot, that it lay on an artificial
392 CHARLES DARWIN
floor of round stones. It seems, therefore, most probable
that at a period when the land stood at a lower level there
was a plain very similar to that now surrounding Callao,
which being protected by a shingle beach, is raised but very
little above the level of the sea. On this plain, with its un-
derlying red-clay beds, I imagine that the Indians manu-
factured their earthen vessels ; and that, during some violent
earthquake, the sea broke over the beach, and converted the
plain into a temporary lake, as happened round Callao in
1713 and 1746. The water would then have deposited mud,
containing fragments of pottery from the kilns, more abun-
dant at some spots than at others, and shells from the sea.
This bed, with fossil earthenware, stands at about the
same height with the shells on the lower terrace of San
Lorenzo, in which the cotton-thread and other relics were
embedded.
Hence we may safely conclude, that within the Indo-human
period there has been an elevation, as before alluded to, of
more than eighty-five feet; for some little elevation must
have been lost by the coast having subsided since the old
maps were engraved. At Valparaiso, although in the 220
years before our visit, the elevation cannot have exceeded
nineteen feet, yet subsequently to 1817, there has been a rise,
partly insensible and partly by a start during the shock of
1822, of ten or eleven feet. The antiquity of the Indo-human
race here, judging by the eighty-five feet rise of the land
: since the relics were embedded, is the more remarkable, as on
the coast of Patagonia, when the land stood about the same
number of feet lower, the Macrauchenia was a living beast;
but as the Patagonian coast is some way distant from the
Cordillera, the rising there may have been slower than here.
At Bahia Blanca, the elevation has been only a few feet
since the numerous gigantic quadrupeds were there en-
tombed; and, according to the generally received opinion,
when these extinct animals were living, man did not exist.
But the rising of that part of the coast of Patagonia, is per-
haps no way connected with the Cordillera, but rather with
a line of old volcanic rocks in Banda Oriental, so that it
may have been infinitely slower than on the shores of Peru.
All these speculations, however, must be vague; for who will
THE VOYAGE OF THE BEAGLE 393
pretend to say that there may not have been several periods
of subsidence, intercalated between the movements of ele-
vation; for we know that along the whole coast of Pata-
gonia, there have certainly been many and long pauses in
the upward action of the elevatory forces.
CHAPTER XVII
Galapagos Archipelago
The whole Group Volcanic — Numbers of Craters — Leafless Bushes-
Colony at Charles Island — James Island — Salt-lake in Crater —
Natural History of the Group — Ornithology, curious Finches — Rep-
tiles — Great Tortoises, habits of — Marine Lizard, feeds on Sea-
weed — Terrestrial Lizard, burrowing habits, herbivorous— Impor-
tance of Reptiles in the Archipelago — Fish, Shells, Insects —
Botany — American Type of Organization — Differences in the
Species or Races on different Islands — Tameness of the Birds —
Fear of Man, an acquired Instinct.
QIEPTEMBER 15th.— This archipelago consists of ten
i\ principal islands, of which five exceed the others in
size. They are situated under the Equator, and be-
tween five and six hundred miles westward of the coast of
America. They are all formed of volcanic rocks; a few
fragments of granite curiously glazed and altered by the
heat, can hardly be considered as an exception. Some of
the craters, surmounting the larger islands, are of immense
size, and they rise to a height of between three and four
thousand feet. Their flanks are studded by innumerable
smaller orifices. I scarcely hesitate to affirm, that there
must be in the whole archipelago at least two thousand
craters. These consist either of lava or scoriae, or of finely-
stratified, sandstone-like tuff. Most of the latter are beau-
tifully symmetrical; they owe their origin to eruptions of
volcanic mud without any lava: it is a remarkable circum-
stance that every one of the twenty-eight tuff-craters which
were examined, had their southern sides either much lower
than the other sides, or quite broken down and removed. As
all these craters apparently have been formed when standing
in the sea, and as the waves from the trade wind and the
swell from the open Pacific here unite their forces on the
southern coasts of all the islands, this singular uniformity
394
THE VOYAGE OF THE BEAGLE
395
fn the broken state of the craters, composed of the soft and
yielding tuff, is easify explained.
Considering that these islands are placed directly under
the equator, the climate is far from being excessively hot;
this seems chiefly caused by the singularly low temperature
of the surrounding water, brought here by the great south-
CUlpeDper&r
Wen man I
SOJfiles.
Bind toes I.
Mrborough
Tbwerl
fJamesl
Indefatigable I
Barringtonf^ hatham t
Mbemarlel
Charles 1 ^^ L
ern Polar current. Excepting during one short season, very
little rain falls, and even then it is irregular; but the clouds
generally hang low. Hence, whilst the lower parts of the
islands are very sterile, the upper parts, at a height of a
thousand feet and upwards, possess a damp climate and a
tolerably luxuriant vegetation. This is especially the case
on the windward sides of the islands, which first receive and
condense the moisture from the atmosphere.
In the morning (17th) we landed on Chatham Island,
which, like the others, rises with a tame and rounded out-
line, broken here and there by scattered hillocks, the remains
396 CHARLES DARWIN
of former craters. Nothing could be less inviting than the
first appearance. A broken field of black basaltic lava,
thrown into the most rugged waves, and crossed by great
fissures, is everywhere covered by stunted, sun-burnt brush-
wood, which shows little signs of life. The dry and parched
surface, being heated by the noon-day sun, gave to the air
a close and sultry feeling, like that from a stove : we fancied
even that the bushes smelt unpleasantly. Although I dili-
gently tried to collect as many plants as possible, I suc-
ceeded in getting very few ; and such wretched-looking little
weeds would have better become an arctic than an equatorial
Flora. The brushwood appears, from a short distance, as
leafless as our trees during winter; and it was some time
before I discovered that not only almost every plant was
now in full leaf, but that the greater number were in flower.
The commonest bush is one of the Euphorbiacese : an acacia
and a great odd-looking cactus are the only trees which
afford any shade. After the season of heavy rains, the isl-
ands are said to appear for a short time partially green. The
volcanic island of Fernando Noronha, placed in many re-
spects under nearly similar conditions, is the only other
country where I have seen a vegetation at all like this of
the Galapagos Islands.
The Beagle sailed round Chatham Island, and anchored
in several bays. One night I slept on shore on a part of the
island, where black truncated cones were extraordinarily
numerous: from one small eminence I counted sixty of
them, all surmounted by craters more or less perfect. The
greater number consisted merely of a ring of red scoriae
or slags, cemented together : and their height above the plain
of lava was not more than from fifty to a hundred feet; none
had been very lately active. The entire surface of this part
of the island seems to have been permeated, like a sieve, by
the subterranean vapours: here and there the lava, whilst
soft, has been blown into great bubbles; and in other parts,
the tops of caverns similarly formed have fallen in, leaving
circular pits with steep sides. From the regular form of the
many craters, they gave to the country an artificial appear-
ance, which vividly reminded me of those parts of Stafford-
shire, where the great iron-foundries are most numerous.
THE VOYAGE OF THE BEAGLE 397
The day was glowing hot, and the scrambling over the rough
surface and through the intricate thickets, was very fatigu-
ing; but I was well repaid by the strange Cyclopean scene.
As I was walking along I met two large tortoises, each of
which must have weighed at least two hundred pounds : one
was eating a piece of cactus, and as I approached, it stared
at me and slowly walked away; the other gave a deep hiss,
and drew in its head. These huge reptiles, surrounded by
the black lava, the leafless shrubs, and large cacti, seemed to
my fancy like some antediluvian animals. The few dull-
coloured birds cared no more for me than they did for the
great tortoises.
23rd. — The Beagle proceeded to Charles Island. This ar-
chipelago has long been frequented, first by the bucaniers,
and latterly by whalers, but it is only within the last six
years, that a small colony has been established here. The
inhabitants are between two and three hundred in number;
they are nearly all people of colour, who have been banished
for political crimes from the Republic of the Equator, of
which Quito is the capital. The settlement is placed about
four and a half miles inland, and at a height probably of a
thousand feet. In the first part of the road we passed
through leafless thickets, as in Chatham Island. Higher up,
the woods gradually became greener; and as soon as we
crossed the ridge of the island, we were cooled by a fine
southerly breeze, and our sight refreshed by a green and
thriving vegetation. In this upper region coarse grasses and
ferns abound; but there are no tree-ferns: I saw nowhere
any member of the palm family, which is the more singular,
as 360 miles northward, Cocos Island takes its name from
the number of cocoa-nuts. The houses are irregularly scat-
tered over a flat space of ground, which is cultivated with
sweet potatoes and bananas. It will not easily be imagined
how pleasant the sight of black mud was to us, after having
been so long accustomed to the parched soil of Peru and
northern Chile. The inhabitants, although complaining of
poverty, obtain, without much trouble, the means of sub-
sistence. In the woods there are many wild pigs and goats ;
but the staple article of animal food is supplied by the
tortoises. Their numbers have of course been greatly re-
398 CHARLES DARWIN
duced in this island, but the people yet count on two days'
hunting giving them food for the rest of the week. It is
said that formerly single vessels have taken away as many
as seven hundred, and that the ship's company of a frigate
some years since brought down in one day two hundred
tortoises to the beach.
September 29th. — We doubled the south-west extremity of
Albemarle Island, and the next day were nearly becalmed
between it and Narborough Island. Both are covered with
immense deluges of black naked lava, which have flowed
either over the rims of the great caldrons, like pitch over the
rim of a pot in which it has been boiled, or have burst forth
from smaller orifices on the flanks; in their descent they
have spread over miles of the sea-coast. On both of these
islands, eruptions are known to have taken place; and in
Albemarle, we saw a small jet of smoke curling from the
summit of one of the great craters. In the evening we an-
chored in Bank's Cove, in Albemarle Island. The next
morning I went out walking. To the south of the broken
tuff-crater, in which the Beagle was anchored, there was
another beautifully symmetrical one of an elliptic form; its
longer axis was a little less than a mile, and its depth about
500 feet. At its bottom there was a shallow lake, in the
middle of which a tiny crater formed an islet. The day was
overpoweringly hot, and the lake looked clear and blue : I
hurried down the cindery slope, and, choked with dust,
eagerly tasted the water — but, to my sorrow, I found it salt
as brine.
The rocks on the coast abounded with great black lizards,
between three and four feet long; and on the hills, an ugly
yellowish-brown species was equally common. We saw
many of this latter kind, some clumsily running out of the
way, and others shuffling into their burrows. I shall pres-
ently describe in more detail the habits of both these reptiles.
The whole of this northern part of Albemarle Island is
miserably sterile.
October 8th. — We arrived at James Island: this island, as
well as Charles Island, were long since thus named after our
kings of the Stuart line. Mr. Bynoe, myself, and our serv-
ants were left here for a week, with provisions and a tent,
THE VOYAGE OF THE BEAGLE 399
whilst the Beagle went for water. We found here a party
of Spaniards, who had been sent from Charles Island to dry
fish, and to salt tortoise-meat. About six miles inland, and
at the height of nearly 2000 feet, a hovel had been built in
which two men lived, who were employed in catching tor-
toises, whilst the others were fishing on the coast. I paid
this party two visits, and slept there one night. As in the
other islands, the lower region was covered by nearly leafless
bushes, but the trees were here of a larger growth than else-
where, several being two feet and some even two feet nine
inches in diameter. The upper region being kept damp by
the clouds, supports a green and flourishing vegetation. So
damp was the ground, that there were large beds of a coarse
cyperus, in which great numbers of a very small water-rail
lived and bred. While staying in this upper region, we lived
entirely upon tortoise-meat: the, breast-plate roasted (as the
Gauchos do came con cueroyf 'with the flesh on it, is very
good; and the young tortoises make excellent soup; but
otherwise the meat to my taste is indifferent.
One day we accompanied a party of the Spaniards in
their whale-boat to a salina, or lake from which salt is pro-
cured. After landing, we had a very rough walk over a
rugged field of recent lava, which has almost surrounded a
tuff-crater, at the bottom of which the salt-lake lies. The
water is only three or four inches deep, and rests on a layer
of beautifully crystallized, white salt. The lake is quite cir-
cular, and is fringed with a border of bright green succulent
plants; the almost precipitous walls of the crater are clothed
with wood, so that the scene was altogether both picturesque
and curious. A few years since, the sailors belonging to a
sealing-vessel murdered their captain in this quiet spot; and
we saw his skull lying among the bushes.
During the greater part of our stay of a week, the sky
was cloudless, and if the trade-wind failed for an hour, the
heat became very oppressive. On two days, the thermometer
within the tent stood for some hours at 93 ° ; but in the open
air, in the wind and sun, at only 85 °. The sand was ex-
tremely hot; the thermometer placed in some of a brown
colour immediately rose to 137°, and how much above that
it would have risen, I do not know, for it was not gradu-
400 CHARLES DARWIN
ated any higher. The black sand felt much hotter, so that
even in thick boots it was quite disagreeable to walk over it.
The natural history of these islands is eminently curious,
and well deserves attention. Most of the organic productions
are aboriginal creations, found nowhere else; there is even
a difference between the inhabitants of the different islands;
yet all show a marked relationship with those of America,
though separated from that continent by an open space of
ocean, between 500 and 600 miles in width. The archipelago
is a little world within itself, or rather a satellite attached to
America, whence it has derived a few stray colonists, and
has received the general character of its indigenous produc-
tions. Considering the small size of the islands, we feel
the more astonished at the number of their aboriginal beings,
and at their confined range. Seeing every height crowned
with its crater, and the boundaries of most of the lava-
streams still distinct, we are led to believe that within a
period geologically recent the unbroken ocean was here
spread out. Hence, both in space and time, we seem to be
brought somewhat near to that great fact — that mystery of
mysteries — the first appearance of new beings on this earth.
Of terrestrial mammals, there is only one which must be
considered as indigenous, namely, a mouse (Mus Galapa-
goensis), and this is confined, as far as I could ascertain, to
Chatham Island, the most easterly island of the group. It
belongs, as I am informed by Mr. Waterhouse, to a division
of the family of mice characteristic of America. At James
Island, there is a rat sufficiently distinct from the common
kind to have been named and described by Mr. Waterhouse ;
but as it belongs to the old-world division of the family, and
as this island has been frequented by ships for the last hun-
dred and fifty years, I can hardly doubt that this rat is
merely a variety produced by the new and peculiar climate,
food, and soil, to which it has been subjected. Although no
one has a right to speculate without distinct facts, yet even
with respect to the Chatham Island mouse, it should be borne
in mind, that it may possibly be an American species im-
ported here; for I have seen, in a most unfrequented part of
the Pampas, a native mouse living in the roof of a newly
THE VOYAGE OF THE BEAGLE 401
built hovel, and therefore its transportation in a vessel is
not improbable: analogous facts have been observed by Dr.
Richardson in North America. — — — -
Of land-birds I obtained twenty-six kinds, all peculiar to
the group and found nowhere else, with the exception of one
lark-like finch from North America (Dolichonyx oryzivorus),
which ranges on that continent as far north as 54 , and gen-
erally frequents marshes. The other twenty-five birds con-
sist, firstly, of a hawk, curiously intermediate in structure
between a buzzard and the American group of carrion-feed-
ing Polybori; and with these latter birds it agrees most
closely in every habit and even tone of voice. Secondly,
there are two owls, representing the short-eared and white
barn-owls of Europe. Thirdly, a wren, three tyrant-flycatch-
ers (two of them species of Pyrocephalus, one or both of
which would be ranked by some ornithologists as only varie-
ties), and a dove — all analogous to, but distinct from, Amer-
ican species. Fourthly, a swallow, which though differing
from the Progne purpurea of both Americas, only in being
rather duller colored, smaller, and slenderer, is considered
by Mr. Gould as specifically distinct. Fifthly, there are three
species of mocking thrush — a form highly characteristic of
America. The remaining land-birds form a most singular
group of finches, related to each other in the structure of
their beaks, short tails, form of body and plumage : there are
thirteen species, which Mr. Gould has divided into four sub-
groups. All these species are peculiar to this archipelago;
and so is the whole group, with the exception of one species
of the sub-group Cactornis, lately brought from Bow Island,
in the Low Archipelago. Of Cactornis, the two species may
be often seen climbing about the flowers of the great cactus-
trees ; but all the other species of this group of finches,
mingled together in flocks, feed on the dry and sterile ground
of the lower districts. The males of all, or certainly of the
greater number, are jet black; and the females (with perhaps
one or two exceptions) are brown. The most curious fact is
the perfect gradation in the size of the beaks in the different
species of Geospiza, from one as large as that of a hawfinch
to that of a chaffinch, and (if Mr. Gould is right in includ-
ing his sub-group, Certhidea, in the main group) even to
402
CHARLES DARWIN
that of a warbler. The largest beak in the genus Geospiza
is shown in Fig. I, and the smallest in Fig. 3; but instead of
there being only one intermediate species, with a beak of
the size shown in Fig. 2, there are no less than six species
with insensibly graduated beaks. The beak of the sub-group
Certhidea, is shown in Fig. 4. The beak of Cactornis is
1. Geospiza magnirostris.
3. Geospiza parvula.
2. Geospiza fortis.
4. Certhidea olivasea.
somewhat like that of a starling; and that of the fourth sub-
group, Camarhynchus, is slightly parrot-shaped. Seeing this
gradation and diversity of structure in one small, intimately
related group of birds, one might really fancy that from an
original paucity of birds in this archipelago, one species had
been taken and modified for different ends. In a like manner
it might be fancied that a bird originally a buzzard, had been
induced here to undertake the office of the carrion-feeding
Polybori of the American continent.
Of waders and water-birds I- was able to get only eleven
kinds, and of these only three (including a rail confined to
the damp summits of the islands) are new species. Consid-
ering the wandering habits of the gulls, I was surprised to
find that the species inhabiting these islands is peculiar, but
allied to one from the southern parts of South America.
THE VOYAGE OF THE BEAGLE 403
The far greater peculiarity of the land-birds, namely, twenty-
five out of twenty-six, being new species, or at least new
races, compared with the waders and web-footed birds, is
in accordance with the greater range which these latter
orders have in all parts of the world. We shall hereafter
see this law of aquatic forms, whether marine or fresh-
water, being less peculiar at any given point of the earth's
surface than the terrestrial forms of the same classes,
strikingly illustrated in the shells, and in a lesser degree in
the insects of this archipelago.
Two of the waders are rather smaller than the same spe-
cies brought from other places: the swallow is also smaller,
though it is doubtful whether or not it is distinct from its
analogue. The two owls, the two tyrant-catchers (Pyo-
cephalus) and the dove, are also smaller than the analogous
but distinct species, to which they are most nearly related;
on the other hand, the gull is rather larger. The two owls,
the swallow, all three species of mocking-thrush, the dove
in its separate colours though not in its whole plumage, the
Totanus, and the gull, are likewise duskier coloured than
their analogous species; and in the case of the mocking-
thrush and Totanus, than any other species of the two gen-
era. With the exception of a wren with a fine yellow breast,
and of a tyrant-flycatcher with a scarlet tuft and breast, none
of the birds are brilliantly coloured, as might have been ex-
pected in an equatorial district. Hence it would appear
probable, that the same causes which here make the im-
migrants of some peculiar species smaller, make most of the
peculiar Galapageian species also smaller, as well as very
generally more dusky coloured. All the plants have a
wretched, weedy appearance, and I did not see one beautiful
flower. The insects, again, are small-sized and dull-coloured,
and, as Mr. Waterhouse informs me, there is nothing in their
general appearance which would have led him to imagine
that they had come from under the equator. 1 The birds,
1 The progress of research has shown that some of these birds, which were
then thought to be confined to the islands, occur on the American continent.
The eminent ornithologist, Mr. Sclater, informs me that this is the ease
with the Strix punctatissima and Pyrocephalus nanus; and probably with
the Otus Galapagoensis and Zenaida Galapagoensis : so that the number of
endemic birds is reduced to twenty-three, or probably to twenty-one. Mr.
Sclater thinks that one or two of these endemic forms should be ranked
rather as varieties than species, which always seemed to me probable.
404 CHARLES DARWIN
plants, and insects have a desert character, and are not more
brilliantly coloured than those from southern Patagonia ; we
may, therefore, conclude that the usual gaudy colouring of
the inter-tropical productions, is not related either to the
heat or light of those zones, but to some other cause, per-
haps to the conditions of existence being generally favour-
able to life.
We will now turn to the order of reptiles, which gives
the most striking character to the zoology of these islands.
The species are not numerous, but the numbers of individ-
uals of each species are extraordinarily great. There is one
small lizard belonging to a South American genus, and two
species (and probably more) of the Amblyrhynchus — a genus
confined to the Galapagos Islands. There is one snake which
is numerous; it is identical, as I am informed by M. Bibron,
with the Psammophis Temminckii from Chile: 2 Of sea-
turtle I believe there are more than one species; and of tor-
toises there are, as we shall presently show, two or three
species or races. Of toads and frogs there are none: I was
surprised at this, considering how well suited for them the
temperate and damp upper woods appeared to be. It re-
called to my mind the remark made by Bory St. Vincent,*
namely, that none of this family are found on any of the vol-
canic islands in the great oceans. As far as I can ascertain
from various works, this seems to hold good throughout the
Pacific, and even in the large islands of the Sandwich archi-
pelago. Mauritius offers an apparent exception, where I
saw the Rana Mascariensis in abundance: this frog is said
now to inhabit the Seychelles, Madagascar, and Bourbon;
but on the other hand, Du Bois, in his voyage in 1669, states
that there were no reptiles in Bourbon except tortoises ; and
the Officier du Roi aserts that before 1768 it had been at-
tempted, without success, to introduce frogs into Mauritius
— I presume for the purpose of eating: hence it may be well
3 This is stated by Dr. Gunther (Zoolog. Soc, Jan 24th, 1859) to be a
peculiar species, not known to inhabit any other country.
3 Voyage aux Quatre lies d'Afrique. With respect to the Sandwich
Islands, see Tyerman and Bennett's Journal, vol. i. p. 434. For Mauritius,
see Voyage par un Officier, etc., part i. p. 170. There are no frogs in the
Canary Islands (Webb et Berthelot, Hist. Nat. des lies Canaries). I saw
none at St. Jago in the Cape de Verds. There are none at St. Helena.
THE VOYAGE OF THE BEAGLE 405
doubted whether this frog is an aboriginal of these islands.
The absence of the frog family in the oceanic islands is the
more remarkable, when contrasted with the case of lizards,
which swarm on most of the smallest islands. May this dif-
ference not be caused, by the greater facility with which the
eggs of lizards, protected by calcareous shells, might be
transported through salt-water, than could the slimy spawn
of frogs?
I will first describe the habits of the tortoise (Testudo
nigra, formerly called Indica), which has been so frequently
alluded to. These animals are found, I believe, on all the
islands of the archipelago; certainly on the greater number.
They frequent in preference the high damp parts, but they
likewise live in the lower and arid districts. I have already
shown, from the numbers which have been caught in a single
day, how very numerous they must be. Some grow to an
immense size: Mr. Lawson, an Englishman, and vice-gov-
ernor of the colony, told us that he had seen several so large,
that it required six or eight men to lift them from the
ground ; and that some had afforded as much as two hundred
pounds of meat. The old males are the largest, the females
rarely growing to so great a size: the male can readily be
distinguished from the female by the greater length of its
tail. The tortoises which live on those islands where there
is no water, or in the lower and arid parts of the others, feed
chiefly on the succulent cactus. Those which frequent the
higher and damp regions, eat the leaves of various trees, a
kind of berry (called guayavita) which is acid and austere,
and likewise a pale green filamentous lichen (Usnera plicata),
that hangs from the boughs of the trees.
The tortoise is very fond of water, drinking large quan-
tities, and wallowing in the mud. The larger islands alone
possess springs, and these are always situated towards the
central parts, and at a considerable height. The tortoises,
therefore, which frequent the lower districts, when thirsty,
are obliged to travel from a long distance. Hence broa d and
well-beaten paths branch off in every direction from the
wells down to the sea-coast; and the Spaniards by following
them up, first discovered the watering-places. When I landed
at Chatham Island, I could not imagine what animal travelled
406 CHARLES DARWIN
so methodically along well-chosen tracks. Near the springs
it was a curious spectacle to behold many of these huge
creatures, one set eagerly travelling onwards with out-
stretched necks, and another set returning, after having
drunk their fill. When the tortoise arrives at the spring,
quite regardless of any spectator, he buries his head in the
water above his eyes, and greedily swallows great mouthfuls,
at the rate of about ten in a minute. The inhabitants say
each animal stays three or four days in the neighbourhood
of the water, and then returns to the lower country; but
they differed respecting the frequency of these visits. The
animal probably regulates them according to the nature of
the food on which it has lived. It is, however, certain, that
tortoises can subsist even on these islands where there is no
other water than what falls during a few rainy days in the
year.
I believe it is well ascertained, that the bladder of the frog
acts as a reservoir for the moisture necessary to its exist-
ence : such seems to be the case with the tortoise. For some
time after a visit to the springs, their urinary bladders are
distended with fluid, which is said gradually to decrease in
volume, and to become less pure. The inhabitants, when
walking in the lower district, and overcome with thirst, often
take advantage of this circumstance, and drink the contents
of the bladder if full : in one I saw killed, the fluid was quite
limpid, and had only a very slightly bitter taste. The inhabit-
ants, however, always first drink the water in the pericar-
dium, which is described as being best.
The tortoises, when purposely moving towards any point,
travel by night and day, and arrive at their journey's end
much sooner than would be expected. The inhabitants, from
observing marked individuals, consider that they travel a
distance of about eight miles in two or three days. One large
tortoise, which I watched, walked at the rate of sixty yards
in ten minutes, that is 360 yards in the hour, or four miles a
day, — allowing a little time for it to eat on the road. During
the breeding season, when the male and female are together,
the male utters a hoarse roar or bellowing, which, it is said,
can be heard at the distance of more than a hundred yards.
The female never uses her voice, and the male only at these
THE VOYAGE OF THE BEAGLE 407
times; so that when the people hear this noise, they know
that the two are together. They were at this time (October)
laying their eggs. The female, where the soil is sandy, de-
posits them together, and covers them up with sand ; but
where the ground is rocky she drops them indiscriminately
in any hole : Mr. Bynoe found seven placed in a fissure. The
egg is white and spherical ; one which I measured was seven
inches and three-eighths in circumference, and therefore
larger than a hen's egg. The young tortoises, as soon as they
are hatched, fall a prey in great numbers to the carrion-
feeding buzzard. The old ones seem generally to die from
accidents, as from falling down precipices : at least, several
of the inhabitants told me, that they never found one dead
without some evident cause.
The inhabitants believe that these animals are absolutely
deaf; certainly they do not overhear a person walking close
behind them. I was always amused when overtaking one of
these great monsters, as it was quietly pacing along, to see
how suddenly, the instant I passed, it would draw in its head
and legs, and uttering a deep hiss fall to the ground with a
heavy sound, as if struck dead. I frequently got on their
backs, and then giving a few raps on the hinder part of their
shells, they would rise up and walk away; — but I found it
very difficult to keep my balance. The flesh of this animal is
largely employed, both fresh and salted; and a beautifully
clear oil is prepared from the fat. When a tortoise is caught,
the man makes a slit in the skin near its tail, so as to see
inside its body, whether the fat under the dorsal plate is
thick. If it is not, the animal is liberated and it is said to
recover soon from this strange operation. In order to secure
the tortoise, it is not sufficient to turn them like turtle, for
they are often able to get on their legs again.
There can be little doubt that this tortoise is an aboriginal
inhabitant of the Galapagoes ; for it is found on all, or nearly
all, the islands, even on some of the smaller ones where there
is no water; had it been an imported species, this would
hardly have been the case in a group which has been so little
frequented. Moreover, the old Bucaniers found this tortoise
in greater numbers even than at present : Wood and Rogers
also, in 1708, say that it is the opinion of the Spaniards, that
408
CHARLES DARWIN
it is found nowhere else in this quarter of the world. It is
now widely distributed; but it may be questioned whether
it is in any other place an aboriginal. The bones of a tor-
toise at Mauritius, associated with those of the extinct Dodo,
have generally been considered as belonging to this tortoise ;
if this had been so, undoubtedly it must have been there
indigenous; but M. Bibron informs me that he believes that
it was distinct, as the species now living there certainly is.
The Amblyrhynchus, a remarkable genus of lizards, is con-
fined to this archipelago; there are two species, resembling
Amblyrhynchus cristatus. a, Tooth of, natural size, and likewise magnified.
each other in general form, one being terrestrial and the
other aquatic. This latter species (A. cristatus) was first
characterized by Mr. Bell, who well foresaw, from its short,
broad head, and strong claws of equal length, that its habits
of life would turn out very peculiar, and different from those
of its nearest ally, the Iguana. It is extremely common on all
the islands throughout the group, and lives exclusively on the
rocky sea-beaches, being never found, at least I never saw
one, even ten yards in-shore. It is a hideous-looking crea-
ture, of a dirty black colour, stupid, and sluggish in its move-
ments. The usual length of a full-grown one is about a yard,
but there are some even four feet long ; a large one weighed
twenty pounds: on the island of Albemarle they seem to
grow to a greater size than elsewhere. Their tails are flat-
tened sideways, and all four feet partially webbed. They are
occasionally seen some hundred yards from the shore,
swimming about; and Captain Collnett, in his Voyage says,
THE VOYAGE OF THE BEAGLE 409
" They go to sea in herds a-fishing, and sun themselves on
the rocks; and may be called alligators in miniature." It
must not, however, be supposed that they live on fish. When
in the water this lizard swims with perfect ease and quick-
ness, by a serpentine movement of its body and flattened tail
— the legs being motionless and closely collapsed on its sides.
A seaman on board sank one, with a heavy weight attached
to it, thinking thus to kill it directly ; but when, an hour after-
wards, he drew up the line, it was quite active. Their limbs
and strong claws are admirably adapted for crawling over the
rugged and fissured masses of lava, which everywhere form
the coast. In such situations, a group of six or seven of
these hideous reptiles may oftentimes be seen on the black
rocks, a few feet above the surf, basking in the sun with out-
stretched legs.
I opened the stomachs of several, and found them largely
distended with minced sea-weed (Ulvae), which grows in
thin foliaceous expansions of a bright green or a dull red
colour. I do not recollect having observed this sea-weed in
any quantity on the tidal rocks ; and I have reason to believe
it grows at the bottom of the sea, at some little distance from
the coast. If such be the case, the object of these animals
occasionally going out to sea is explained. The stomach con-
tained nothing but the sea-weed. Mr. Baynoe, however, found
a piece of crab in one; but this might have got in acci-
dentally, in the same manner as I have seen a caterpillar, in
the midst of some lichen, in the paunch of a tortoise. The
intestines were large, as in other herbivorous animals. The
nature of this lizard's food, as well as the structure of its
tail and feet, and the fact of its having been seen voluntarily
swimming out at sea, absolutely prove its aquatic habits;
yet there is in this respect one strange anomaly, namely, that
when frightened it will not enter the water. Hence it is
easy to drive these lizards down to any little point overhang-
ing the sea, where they will sooner allow a person to catch
hold of their tails than jump into the water. They do not
seem to have any notion of biting ; but when much frightened
they squirt a drop of fluid from each nostril. I threw one
several times as far as I could, into a deep pool left by the
retiring tide; but it invariably returned in a direct line to
410 CHARLES DARWIN
the spot where I stood. It swam near the bottom, with a
very graceful and rapid movement, and occasionally aided
itself over the uneven ground with its feet. As soon as it
arrived near the edge, but still being under water, it tried to
conceal itself in the tufts of sea-weed, or it entered some
crevice. As soon as it thought the danger was past, it
crawled out on the dry rocks, and shuffled away as quickly
as it could. I several times caught this same lizard, by driv-
ing it down to a point, and though possessed of such perfect
powers of diving and swimming, nothing would induce it to
enter the water ; and as often as I threw it in, it returned in
the manner above described. Perhaps this singular piece of
apparent stupidity may be accounted for by the circum-
stance, that this reptile has no enemy whatever on shore,
whereas at sea it must often fall a prey to the numerous
sharks. Hence, probably, urged by a fixed and hereditary
instinct that the shore is its place of safety, whatever the
emergency may be, it there takes refuge.
During our visit (in October), I saw extremely few small
individuals of this species, and none I should think under
a year old. From this circumstance it seems probable that
the breeding season had not then commenced. I asked sev-
eral of the inhabitants if they knew where it laid its eggs:
they said that they knew nothing of its propagation, although
well acquainted with the eggs of the land kind — a fact, con-
sidering how very common this lizard is, not a little extra-
ordinary.
We will now turn to the terrestrial species (A. Demarlii),
with a round tail, and toes without webs. This lizard,
instead of being found like the other on all the islands, is
confined to the central part of the archipelago, namely to
Albemarle, James, Barrington, and Indefatigable islands. To
the southward, in Charles, Hood, and Chatham islands, and
to the northward, in Towers, Bindloes, and Abingdon, I
neither saw nor heard of any. It would appear as if it had
been created in the centre of the archipelago, and thence had
been dispersed only to a certain distance. Some of these
lizards inhabit the high and damp parts of the islands, but
they are much more numerous in the lower and sterile
districts near the coast. I cannot give a more forcible proof
THE VOYAGE OF THE BEAGLE 411
of their numbers, than by stating that when we were left at
James Island, we could not for some time find a spot free
from their burrows on which to pitch our single tent. Like
their brothers the sea-kind, they are ugly animals, of a yellow-
ish orange beneath, and of a brownish red colour above:
from their low facial angle they have a singularly stupid
appearance. They are, perhaps, of a rather less size than the
marine species; but several of them weighed between ten and
fifteen pounds. In their movements they are lazy and half
torpid. When not frightened, they slowly crawl along with
their tails and bellies dragging on the ground. They often
stop, and doze for a minute or two, with closed eyes and hind
legs spread out on the parched soil.
They inhabit burrows, which they sometimes make between
fragments of lava, but more generally on level patches of the
soft sandstone-like tuff. The holes do not appear to be very
deep, and they enter the ground at a small angle; so that
when walking over these lizard-warrens, the soil is constantly
giving way, much to the annoyance of the tired walker. This
animal, when making its burrow, works alternately the oppo-
site sides of its body. One front leg for a short time
scratches up the soil, and throws it towards the hind foot,
which is well placed so as to heave it beyond the mouth of
the hole. That side of the body being tired, the other takes
up the task, and so on alternately. I watched one for a long
time, till half its body was buried ; I then walked up and pulled
it by the tail; at this it was greatly astonished, and soon
shuffled up to see what was the matter; and then stared me
in the face, as much as to say, "What made you pull my
tail?"
They feed by day, and do not wander far from their bur-
rows ; if frightened, they rush to them with a most awkward
gait. Except when running down hill, they cannot move
very fast, apparently from the lateral position of their legs.
They are not at all timorous. : when attentively watching any
one, they curl their tails, and, raising themselves on their
front legs, nod their heads vertically, with a quick movement,
and try to look very fierce ; but in reality they are not at all
so: if one just stamps on the ground, down go their tails,
and off they shuffle as quickly as they can. I have frequently
412 CHARLES DARWIN
observed small fly-eating lizards, when watching anything,
nod their heads in precisely the same manner; but I do not
at all know for what purpose. If this Amblyrhynchus is held
and plagued with a stick, it will bite it very severely; but
I caught many by the tail, and they never tried to bite me.
If two are placed on the ground and held together, they will
fight, and bite each other till blood is drawn.
The individuals, and they are the greater number, which
inhabit the lower country, can scarcely taste a drop of water
throughout the year; but they consume much of the succulent
cactus, the branches of which are occasionally broken off
by the wind. I several times threw a piece to two or three
of them when together; and it was amusing enough to see
them trying to seize and carry it away in their mouths, like
so many hungry dogs with a bone. They eat very deliber-
ately, but do not chew their food. The little birds are aware
how harmless these creatures are: I have seen one of the
thick-billed finches picking at one end of a piece of cactus
(which is much relished by all the animals of the lower
region), whilst a lizard was eating at the other end; and
afterwards the little bird with the utmost indifference hopped
on the back of the reptile.
I opened the stomachs of several, and found them full of
vegetable fibres and leaves of different trees, especially of
an acacia. In the upper region they live chiefly on the acid
and astringent berries of the guayavita, under which trees
I have seen these lizards and the huge tortoises feeding
together. To obtain the acacia-leaves they crawl up the low
stunted trees ; and it is not uncommon to see a pair quietly
browsing, whilst seated on a branch several feet above the
ground. These lizards, when cooked, yield a white meat,
which is liked by those whose stomachs soar above all
prejudices.
Humboldt has remarked that in intertropical South
America, all lizards which inhabit dry regions are esteemed
delicacies for the table. The inhabitants state that those
which inhabit the upper damp parts drink water, but that
the others do not, like the tortoises, travel up for it from
the lower sterile country. At the time of our visit, the
females had within their bodies numerous, large, elongated
THE VOYAGE OF THE BEAGLE 413
e gg s , which they lay in their burrows: the inhabitants seek
them for food.
These two species of Amblyrhynchus agree, as I have
already stated, in their general structure, and in many of
their habits. Neither have that rapid movement, so charac-
teristic of the genera Lacerta and Iguana. They are both
herbivorous, although the kind of vegetation on which they
feed is so very different. Mr. Bell has given the name to the
genus from the shortness of the snout: indeed, the form of
the mouth may almost be compared to that of the tortoise:
one is led to suppose that this is an adaptation to their
herbivorous appetites. It is very interesting thus to find a
well-characterized genus, having its marine and terrestrial
species, belonging to so confined a portion of the world. The
aquatic species is by far the most remarkable, because it is
the only existing lizard which lives on marine vegetable pro-
ductions. As I at first observed, these islands are not so
remarkable for the number of the species of reptiles, as for
that of the individuals; when we remember the well-beaten
paths made by the thousands of huge tortoises — the many
turtles — the great warrens of the terrestrial Amblyrhynchus
— and the groups of the marine species basking on the coast-
rocks of every island — we must admit that there is no other
quarter of the world where this Order replaces the herbivo-
rous mammalia in so extraordinary a manner. The geologist
on hearing this will probably refer back in his mind to the
Secondary epochs, when lizards, some herbivorous, some
carnivorous, and of dimensions comparable only with our
existing whales, swarmed on the land and in the sea. It is,
therefore, worthy of his observation, that this archipelago,
instead of possessing a humid climate and rank vegetation,
cannot be considered otherwise than extremely arid, and, for
an equatorial region, remarkably temperate.
To finish with the zoology: the fifteen kinds of sea-fish
which I procured here are all new species; they belong to
twelve genera, all widely distributed, with the exception of
Prionotus, of which the four previously known species live
on the eastern side of America. Of land-shells I collected
sixteen kinds (and two marked varieties), of which, with the
exception of one Helix found at Tahiti, all are peculiar to
414 CHARLES DARWIN
this archipelago: a single fresh-water shell (Paludina) is
common to Tahiti and Van Diemen's Land. Mr. Cuming,
before our voyage, procured here ninety species of sea-shells,
and this does not include several species not yet specifically
examined, of Trochus, Turbo, Monodonta, and Nassa. He
has been kind enough to give me the following interesting
results: Of the ninety shells, no less than forty-seven are
unknown elsewhere — a wonderful fact, considering how
widely distributed sea-shells generally are. Of the forty-
three shells found in other parts of the world, twenty-five
inhabit the western coast of America, and of these eight are
distinguishable as varieties; the remaining eighteen (includ-
ing one variety) were found by Mr. Cuming in the Low
Archipelago, and some of them also at the Philippines. This
fact of shells from islands in the central parts of the Pacific
occurring here, deserves notice, for not one single sea-shell is
known to be common to the islands of that ocean and to the
west coast of America. The space of open sea running north
and south off the west coast, separates two quite distinct
conchological provinces; but at the Galapagos Archipelago
we have a halting-place, where many new forms have been
created, and whither these two great conchological provinces
have each sent up several colonists. The American province
has also sent here representative species ; for there is a Gala-
pageian species of Monoceros, a genus only found on the
west coast of America; and there are Galapageian species
of Fissurella and Cancellaria, genera common on the west
coast, but not found (as I am informed by Mr. Cuming) in
the central islands of the Pacific. On the other hand, there
are Galapageian species of Oniscia and Stylifer, genera com-
mon to the West Indies and to the Chinese and Indian seas,
but not found either on the west coast of America or in the
central Pacific. I may here add, that after the comparison
by Messrs. Cuming and Hinds of about 2000 shells from
the eastern and western coasts of America, only one single
shell was found in common, namely, the Purpura patula,
which inhabits the West Indies, the coast of Panama,
and the Galapagos. We have, therefore, in this quarter
of the world, three great conchological sea-provinces, quite
distinct, though surprisingly near each other, being sepa-
THE VOYAGE OF THE BEAGLE 415
rated by long north and south spaces either of land or of
open sea.
I took great pains in collecting the insects, but excepting
Tierra del Fuego, I never saw in this respect so poor a coun-
try. Even in the upper and damp region I procured very few,
excepting some minute Diptera and Hymenoptera, mostly of
common mundane forms. As before remarked, the insects,
for a tropical region, are of very small size and dull colours.
Of beetles I collected twenty-five species (excluding a Der-
mestes and Corynetes imported, wherever a ship touches) ;
of these, two belong to the Harpalidae, two to the Hydro-
philidse, nine to three families of the Heteromera, and the
remaining twelve to as many different families. This cir-
cumstance of insects (and I may add plants), where few in
number, belonging to many different families, is, I believe,
very general. Mr. Waterhouse, who has published 4 an
account of the insects of this archipelago, and to whom I am
indebted for the above details, informs me that there are
several new genera: and that of the genera not new, one
or two are American, and the rest of mundane distribution.
With the exception of a wood-feeding Apate, and of one or
probably two water-beetles from the American continent,
all the species appear to be new.
The botany of this group is fully as interesting as the
zoology. Dr. J. Hooker will soon publish in the " Linnean
Transactions " a full account of the Flora, and I am much
indebted to him for the following details. Of flowering
plants there are, as far as at present is known, 185 species,
and 40 cryptogamic species, making altogether 225; of this
number I was fortunate enough to bring home 193. Of the
flowering plants, 100 are new species, and are probably con-
fined to this archipelago. Dr. Hooker conceives that, of the
plants not so confined, at least 10 species found near the
cultivated ground at Charles Island, have been imported.
It is, I think, surprising that more American species have
not been introduced naturally, considering that the distance
is only between 500 and 600 miles from the continent; and
that (according to Collnet, p. 58) drift-wood, bamboos, canes,
and the nuts of a palm, are often washed on the south-eastern
4 Ann. and Mag. of Nat. Hist., vol. xvi. p. 19.
416 CHARLES DARWIN
shores. The proportion of ioo flowering plants out of 185
(or 175 excluding the imported weeds) being new, is suffi-
cient, I conceive, to make the Galapagos Archipelago a dis-
tinct botanical province ; but this Flora is not nearly so
peculiar as that of St. Helena, nor, as I am informed by
Dr. Hooker, of Juan Fernandez. The peculiarity of the
Galapageian Flora is best shown in certain families; — thus
there are 21 species of Composite, of which 20 are peculiar
to this archipelago; these belong to twelve genera, and of
these genera no less than ten are confined to the archipelago !
Dr. Hooker informs me that the Flora has an undoubtedly
Western American character; nor can he detect in it any
affinity with that of the Pacific. If, therefore, we except the
eighteen marine, the one fresh-water, and one land-shell,
which have apparently come here as colonists from the
central islands of the Pacific, and likewise the one distinct
Pacific species of the Galapageian group of finches, we see
that this archipelago, though standing in the Pacific Ocean,
is zoologically part of America.
If this character were owing merely to immigrants from
America, there would be little remarkable in it; but we see
that a vast majority of all the land animals, and that more
than half of the flowering plants, are aboriginal productions.
It was most striking to be surrounded by new birds, new rep-
tiles, new shells, new insects, new plants, and yet by innumer-
able trifling details of structure, and even by the tones of
voice and plumage of the birds, to have the temperate plains
of Patagonia, or rather the hot dry deserts of Northern Chile,
vividly brought before my eyes. Why, on these small points
of land, which within a late geological period must have
been covered by the ocean, which are formed by basaltic lava,
and therefore differ in geological character from the Ameri-
can continent, and which are placed under a peculiar climate,
— why were their aboriginal inhabitants, associated, I may
add, in different proportions both in kind and number from
those on the continent, and therefore acting on each other
in a different manner — why were they created on American
types of organization? It is probable that the islands of the
Cape de Verd group resemble, in all their physical conditions,
far more closely the Galapagos Islands, than these latter
THE VOYAGE OF THE BEAGLE 417
physically resemble the coast of America, yet the aboriginal
inhabitants of the two groups are totally unlike; those of the
Cape de Verd Islands bearing the impress of Africa, as
the inhabitants of the Galapagos Archipelago are stamped
with that of America.
I have not as yet noticed by far the most remarkable fea-
ture in the natural history of this archipelago; it is, that
the different islands to a considerable extent are inhabited by
a different set of beings. My attention was first called to
this fact by the Vice-Governor, Mr. Lawson, declaring that
the tortoises differed from the different islands, and that he
could with certainty tell from which island any one was
brought. I did not for some time pay sufficient attention
to this statement, and I had already partially mingled to-
gether the collections from two of the islands. I never
dreamed that islands, about 50 or 60 miles apart, and most of
them in sight of each other, formed of precisely the same
rocks, placed under a quite similar climate, rising to a nearly
equal height, would have been differently tenanted; but we
shall soon see that this is the case. It is the fate of most
voyagers, no sooner to discover what is most interesting in
any locality, than they are hurried from it; but I ought, per-
haps, to be thankful that I obtained sufficient materials to
establish this most remarkable fact in the distribution of
organic beings.
The inhabitants, as I have said, state that they can dis-
tinguish the tortoises from the different islands; and that
they differ not only in size, but in other characters. Captain
Porter has described 5 those from Charles and from the near-
est island to it, namely, Hood Island, as having their shells
in front thick and turned up like a Spanish saddle, whilst
the tortoises from James Island are rounder, blacker, and
have a better taste when cooked. M. Bibron, moreover,
informs me that he has seen what he considers two distinct
species of tortoise from the Galapagos, but he does not know
from which islands. The specimens that I brought from
three islands were young ones: and probably owing to this
cause neither Mr. Gray nor myself could find in them any
5 Voyage in the U. S. ship Essex, vol. i. p. .215.
VOL. XXIX — N HC
418 CHARLES DARWIN
specific differences. I have remarked that the marine
Amblyrhynchus was larger at Albemarle Island than else-
where; and M. Bibron informs me that he has seen two dis-
tinct aquatic species of this genus; so that the different
islands probably have their representative species or races
of the Amblyrhynchus, as well as of the tortoise. My atten-
tion was first thoroughly aroused, by comparing together
the numerous specimens, shot by myself and several other
parties on board, of the mocking-thrushes, when, to my aston-
ishment, I discovered that all those from Charles Island
belonged to one species (Mimus trifasciatus) ; all from
Albemarle Island to M. parvulus; and all from James and
Chatham Islands (between which two other islands are sit-
uated, as connecting links) belonged to M. melanotis. These
two latter species are closely allied, and would by some
ornithologists be considered as only well-marked races or
varieties; but the Mimus trifasciatus is very distinct. Un-
fortunately most of the specimens of the finch tribe were
mingled together; but I have strong reasons to suspect that
some of the species of the sub-group Geospiza are confined
to separate islands. If the different islands have their repre-
sentatives of Geospiza, it may help to explain the singularly
large number of the species of this sub-group in this one
small archipelago, and as a probable consequence of their
numbers, the perfectly graduated series in the size of their
beaks. Two species of the sub-group Cactornis, and two of
the Camarhynchus, were procured in the archipelago; and
of the numerous specimens of these two sub-groups shot by
four collectors at James Island, all were found to belong to
one species of each; whereas the numerous specimens shot
either on Chatham or Charles Island (for the two sets were
mingled together) all belonged to the two other species:
hence we may feel almost sure that these islands possess
their respective species of these two sub-groups. In land-
shells this law of distribution does not appear to hold good.
In my very small collection of insects, Mr. Waterhouse
remarks, that of those which were ticketed with their local-
ity, not one was common to any two of the islands.
If we now turn to the Flora, we shall find the aboriginal
plants of the different islands wonderfully different. I give
THE VOYAGE OF THE BEAGLE
419
all the following results on the high authority of my friend
Dr. J. Hooker. I may premise that I indiscriminately col-
lected everything in flower on the different islands, and for-
tunately kept my collections separate. Too much confidence,
however, must not be placed in the proportional results, as
the small collections brought home by some other naturalists,
though in some respects confirming the results, plainly show
that much remains to be done in the botany of this group:
the Leguminosae, moreover, has as yet been only approxi-
mately worked out: —
Name
of
Island.
Total
No. of
Species
No. of
Species
found in
other parts
of the
world.
No. of
Species
confined
to the
Galapagos
Archipel-
ago.
No.
con-
fined
to the
one
Island.
No. of Species
confined to the
Galapagos
Archipelago,
but found on
more than the
one Island.
James Island
Albemarle Island
Chatham Island
Charles Island
7 1
4
32
68
33
18
16
39
(or 29, if the
probably im-
ported plants
be subtracted)
38
26
16
29
30
22
12
21
8
4
4
8
Hence we have the truly wonderful fact, that in James
Island, of the thirty-eight Galapageian plants, or those found
in no other part of the world, thirty are exclusively confined
to this one island; and in Albemarle Island, of the twenty-
six aboriginal Galapageian plants, twenty-two are confined
to this one island, that is, only four are at present known to
grow in the other islands of the archipelago; and so on, as
shown in the above table, with the plants from Chatham and
Charles Islands. This fact will, perhaps, be rendered even
more striking, by giving a few illustrations: — thus, Scalesia,
a remarkable arborescent genus of the Composite, is con-
fined to the archipelago: it has six species: one from Chat-
ham, one from Albemarle, one from Charles Island, two from
James Island, and the sixth from one of the three latter
islands, but it is not known from which : not one of these six
species grows on any two islands. Again, Euphorbia, a mun-
420 CHARLES DARWIN
dane or widely distributed genus, has here eight species, of
which seven are confined to the archipelago, and not one
found on any two islands : Acalypha and Borreria, both mun-
dane genera, have respectively six and seven species, none
of which have the same species on two islands, with the
exception of one Borreria, which does occur on two islands.
The species of the Composite are particularly local ; and Dr.
Hooker has furnished me with several other most striking
illustrations of the difference of the species on the different
islands. He remarks that this law of distribution holds good
both with those genera confined to the archipelago, and those
distributed in other quarters of the world: in like manner
we have seen that the different islands have their proper spe-
cies of the mundane genus of tortoise, and of the widely
distributed American genus of the mocking-thrush, as well
as of two of the Galapageian sub-groups of finches, and
almost certainly of the Galapageian genus Amblyrhynchus.
The distribution of the tenants of this archipelago would
not be nearly so wonderful, if, for instance, one island had
a mocking-thrush, and a second island some other quite dis-
tinct genus; — if one island had its genus of lizard, and a
second island another distinct genus, or none whatever; — or
if the different islands were inhabited, not by representative
species of the same genera of plants, but by totally different
genera, as does to a certain extent hold good: for, to give
one instance, a large berry-bearing tree at James Island has
no representative species in Charles Island. But it is the
circumstance, that several of the islands possess their own
species of the tortoise, mocking-thrush, finches, and numer-
ous plants, these species having the same general habits,
occupying analogous situations, and obviously filling the
same place in the natural economy of this archipelago, that
strikes me with wonder. It may be suspected that some of
these representative species, at least in the case of the tor-
toise and of some of the birds, may hereafter prove to be
only well-marked races; but this would be of equally great
interest to the philosophical naturalist. I have said that most
of the islands are in sight of each other: I may specify that
Charles Island is fifty miles from the nearest part of Chat-
ham Island, and thirty-three miles from the nearest part of
THE VOYAGE OF THE BEAGLE 421
Albemarle Island. Chatham Island is sixty miles from the
nearest part of James Island, but there are two intermediate
islands between them which were not visited by me. James
Island is only ten miles from the nearest part of Albemarle
Island, but the two points where the collections were made
are thirty-two miles apart. I must repeat, that neither the
nature of the soil, nor height of the land, nor the climate,
nor the general character of the associated beings, and there-
fore their action one on another, can differ much in the dif-
ferent islands. If there be any sensible difference in their
climates, it must be between the Windward group (namely,
Charles and Chatham Islands), and that to leeward; but
there seems to be no corresponding difference in the produc-
tions of these two halves of the archipelago.
The only light which I can throw on this remarkable dif-
ference in the inhabitants of the different islands, is, that
very strong currents of the sea running in a westerly and
W.N.W. direction must separate, as far as transportal by the
sea is concerned, the southern islands from the northern
ones ; and between these northern islands a strong N.W. cur-
rent was observed, which must effectually separate James
and Albemarle Islands. As the archipelago is free to a
most remarkable degree from gales of wind, neither the
birds, insects, nor lighter seeds, would be blown from island
to island. And lastly, the profound depth of the ocean be-
tween the islands, and their apparently recent (in a geologi-
cal sense) volcanic origin, render it highly unlikely that they
were ever united ; and this, probably, is a far more important
consideration than any other, with respect to the geographi-
cal distribution of their inhabitants. Reviewing the facts
here given, one is astonished at the amount of creative force,
if such an expression may be used, displayed on these small,
barren, and rocky islands; and still more so, at its diverse
yet analogous action on points so near each other. I have
said that the Galapagos Archipelago might be called a satel-
lite attached to America, but it should rather be called a
group of satellites, physically similar, organically distinct,
yet intimately related to each other, and all related in a
marked, though much lesser degree, to the great American
continent.
422 CHARLES DARWIN
I will conclude my description of the natural history of
these islands, by giving an account of the extreme tameness
of the birds.
This disposition is common to all the terrestrial species;
namely, to the mocking-thrushes, the finches, wrens, tyrant-
flycatchers, the dove, and carrion-buzzard. All of them are
often approached sufficiently near to be killed with a switch,
and sometimes, as I myself tried, with a cap or hat. A gun
is here almost superfluous; for with the muzzle I pushed a
hawk off the branch of a tree. One day, whilst lying down,
a mocking- thrush alighted on the edge of a pitcher, made of
the shell of a tortoise, which I held in my hand, and began
very quietly to sip the water; it allowed me to lift it from
the ground whilst seated on the vessel: I often tried, and
very nearly succeeded, in catching these birds by their legs.
Formerly the birds appear to have been even tamer than at
present. Cowley (in the year 1684) savs tnat the "Turtle-
doves were so tame, that they would often alight on our hats
and arms, so as that we could take them alive ; they not fear-
ing man, until such time as some of our company did fire at
them, whereby they were rendered more shy." Dampier
also, in the same year, says that a man in a morning's walk
might kill six or seven dozen of these doves. At present,
although certainly very tame, they do not alight on people's
arms, nor do they suffer themselves to be killed in such large
numbers. It is surprising that they have not become wilder;
for these islands during the last hundred and fifty years have
been frequently visited by bucaniers and whalers; and the
sailors, wandering through the wood in search of tortoises,
always take cruel delight in knocking down the little birds.
These birds, although now still more persecuted, do not
readily become wild. In Charles Island, which had then
been colonized about six years, I saw a boy sitting by a well
with a switch in his hand, with which he killed the doves
and finches as they came to drink. He had already procured
a little heap of them for his dinner; and he said that he had
constantly been in the habit of waiting by this well for the
same purpose. It would appear that the birds of this archi-
pelago, not having as yet learnt that man is a more danger-
ous animal than the tortoise or the Amblyrhynchus, disregard
THE VOYAGE OF THE BEAGLE 423
him, in the same manner as in England shy birds, such as
magpies, disregard the cows and horses grazing in our fields.
The Falkland Islands offer a second instance of birds
with a similar disposition. The extraordinary tameness of
the little Opetiorhynchus has been remarked by Pernety,
Lesson, and other voyagers. It is not, however, peculiar to
that bird: the Polyborus, snipe, upland and lowland goose,
thrush, bunting, and even some true hawks, are all more or
less tame. As the birds are so tame there, where foxes,
hawks, and owls occur, we may infer that the absence of all
rapacious animals at the Galapagos, is not the cause of their
tameness here. The upland geese at the Falklands show, by
the precaution they take in building on the islets, that they
are aware of their danger from the foxes; but they are not
by this rendered wild towards man. This tameness of the
birds, especially of the waterfowl, is strongly contrasted with
the habits of the same species in Tierra del Fuego, where for
ages past they have been persecuted by the wild inhabitants.
In the Falklands, the sportsman may sometimes kill more
of the upland geese in one day than he can carry home;
whereas in Tierra del Fuego it is nearly as difficult to kill
one, as it is in England to shoot the common wild goose.
In the time of Pernety (1763), all the birds there appear
to have been much tamer than at present; he states that the
Opetiorhynchus would almost perch on his finger; and that
with a wand he killed ten in half an hour. At that period
the birds must have been about as tame as they now are at
the Galapagos. They appear to have learnt caution more
slowly at these latter islands than at the Falklands, where
they have had proportionate means of experience; for be-
sides frequent visits from vessels, those islands have been at
intervals colonized during the entire period. Even formerly,
when all the birds were so tame, it was impossible by Per-
nety's account to kill the black-necked swan — a bird of
passage, which probably brought with it the wisdom learnt
in foreign countries.
I may add that, according to Du Bois, all the birds at
Bourbon in 1571-72, with the exception of the flamingoes
and geese, were so extremely tame, that they could be caught
by the hand, or killed in any number with a stick. Again,
424 CHARLES DARWIN
at Tristan d'Acunha in the Atlantic, Carmichael 6 states that
the only two land-birds, a thrush and a bunting, were " so
tame as to suffer themselves to be caught with a hand-net."
From these several facts we may, I think, conclude, first, that
the wildness of birds with regard to man, is a particular
instinct directed against him, and not dependent upon any
general degree of caution arising from other sources of
danger; secondly, that it is not acquired by individual birds
in a short time, even when much persecuted ; but that in the
course of successive generations it becomes hereditary. With
domesticated animals we are accustomed to see new mental
habits or instincts acquired or rendered hereditary; but with
animals in a state of nature, it must always be most difficult
to discover instances of acquired hereditary knowledge. In
regard to the wildness of birds towards man, there is no way
of accounting for it, except as an inherited habit: compara-
tively few young birds, in any one year, have been injured
by man in England, yet almost all, even nestlings, are afraid
of him; many individuals, on the other hand, both at the
Galapagos and at the Falklands, have been pursued and
injured by man, yet have not learned a salutary dread of
him. We may infer from these facts, what havoc the intro-
duction of any new beast of prey must cause in a country,
before the instincts of the indigenous inhabitants have
become adapted to the stranger's craft or power.
6 Linn. Trans., vol. xii. p. 496. The most anomalous fact on this sub-
ject which I have met with is the wildness of the small birds in the Arctic
parts of North America (as described by Richardson, Fauna Bor., vol. ii.
p. 332), where they are said never to be persecuted. This case is the more
strange, because it is asserted that some of the same species in their winter-
quarters in the United States are tame. There is much, as Dr. Richardson
well remarks, utterly inexplicable connected with the different degrees of
shyness and care with which birds conceal their nests. How strange it
i; that the English wood-pigeon, generally so wild a bird, should very fre-
quently rear its young in shrubberies close to houses!
CHAPTER XVIII
Tahiti and New Zealand
Pass through the Low Archipelago — Tahiti — Aspect — Vegetation on
the Mountains — View of Eimeo — Excursion into the Interior —
Profound Ravines — Succession of Waterfalls — Number of wild
useful Plants — Temperance of the Inhabitants — Their moral state
— Parliament convened — New Zealand — Bay of Islands — Hippahs
— Excursion to Waimate — Missionary Establishment — English
Weeds now run wild — Waiomio — Funeral of a New Zealand
Woman — Sail for Australia.
S~\CTOBER 20th. — The survey of the Galapagos Archi-
f J pelago being concluded, we steered towards Tahiti
and commenced our long passage of 3200 miles. In
the course of a few days we sailed out of the gloomy and
clouded ocean-district which extends during the winter far
from the coast of South America. We then enjoyed bright
and clear weather, while running pleasantly along at the
rate of 150 or 160 miles a day before the steady trade-wind.
The temperature in this more central part of the Pacific is
higher than near the American shore. The thermometer in
the poop cabin, by night and day, ranged between 8o° and
83 , which feels very pleasant; but with one degree or two
higher, the heat becomes oppressive. We passed through
the Low or Dangerous Archipelago, and saw several of
those most curious rings of coral land, just rising above the
water's edge, which have been called Lagoon Islands. A
long and brilliantly white beach is capped by a margin of
green vegetation; and the strip, looking either way, rapidly
narrows away in the distance, and sinks beneath the horizon.
From the mast-head a wide expanse of smooth water can be
seen within the ring. These low hollow coral islands bear
no proportion to the vast ocean out of which they abruptly
rise; and it seems wonderful, that such weak invaders are
not overwhelmed, by the all-powerful and never-tiring waves
of that great sea, miscalled the Pacific.
425
426 CHARLES DARWIN
November 15th. — At daylight, Tahiti, an island which
must for ever remain classical to the voyager in the South
Sea, was in view. At a distance the appearance was not
attractive. The luxuriant vegetation of the lower part could
not yet be seen, and as the clouds rolled past, the wildest
and most precipitous peaks showed themselves towards the
centre of the island. As soon as we anchored in Matavai
Bay, we were surrounded by canoes. This was our Sunday,
but the Monday of Tahiti: if the case had been reversed,
we should not have received a single visit; for the injunction
not to launch a canoe on the sabbath is rigidly obeyed.
After dinner we landed to enjoy all the delights produced
by the first impressions of a new country, and that country
the charming Tahiti. A crowd of men, women, and children,
was collected on the memorable Point Venus, ready to
receive us with laughing, merry faces. They marshalled
us towards the house of Mr. Wilson, the missionary of the
district, who met us on the road, and gave us a very friendly
reception. After sitting a very short time in his house, we
separated to walk about, but returned there in the evening.
The land capable of cultivation, is scarcely in any part
more than a fringe of low alluvial soil, accumulated round
the base of the mountains, and protected from the waves of
the sea by a coral reef, which encircles the entire line of
coast. Within the reef there is an expanse of smooth water,
like that of a lake, where the canoes of the natives can ply
with safety and where ships anchor. The low land which
comes down to the beach of coral-sand, is covered by the
most beautiful productions of the intertropical regions. In
the midst of bananas, orange, cocoa-nut, and bread-fruit
trees, spots are cleared where yams, sweet potatoes, and
sugar-cane, and pine-apples are cultivated. Even the brush-
wood is an imported fruit-tree, namely, the guava, which
from its abundance has 'become as noxious as a weed. In
Brazil I have often admired the varied beauty of the
bananas, palms, and orange-trees contrasted together; and
here we also have the bread-fruit, conspicuous from its large,
glossy, and deeply digitated leaf. It is admirable to behold
groves of a tree, sending forth its branches with the vigour
of an English oak, loaded with large and most nutritious
THE VOYAGE OF THE BEAGLE 427
fruit. However seldom the usefulness of an object can
account for the pleasure of beholding it, in the case of these
beautiful woods, the knowledge of their high productiveness
no doubt enters largely into the feeling of admiration. The
little winding paths, cool from the surrounding shade, led
to the scattered houses ; the owners of which everywhere
gave us a cheerful and most hospitable reception.
I was pleased with nothing so much as with the inhabit-
ants. There is a mildness in the expression of their coun-
tenances which at once banishes the idea of a savage; and
an intelligence which shows that they are advancing in civili-
zation. The common people, when working, keep the upper
part of their bodies quite naked; and it is then that the
Tahitians are seen to advantage. They are very tall, broad-
shouldered, athletic, and well-proportioned. It has been
remarked, that it requires little habit to make a dark skin
more pleasing and natural to the eye of an European than
his own colour. A white man bathing by the side of a
Tahitian, was like a plant bleached by the gardener's art
compared with a fine dark green one growing vigorously in
the open fields. Most of the men are tattooed, and the orna-
ments follow the curvature of the body so gracefully, that
they have a very elegant effect. One common pattern, vary-
ing in its details, is somewhat like the crown of a palm-tree.
It springs from the central line of the back, and gracefully
curls round both sides. The simile may be a fanciful one,
but I thought the body of a man thus ornamented was like
the trunk of a noble tree embraced by a delicate creeper.
Many of the elder people had their feet covered with
small figures, so placed as to resemble a sock. This fashion,
however, is partly gone by, and has been succeeded by others.
Here, although fashion is far from immutable, every one
must abide by that prevailing in his youth. An old man
has thus his age for ever stamped on his body, and he cannot
assume the airs of a young dandy. The women are tattooed
in the same manner as the men, and very commonly on their
fingers. One unbecoming fashion is now almost universal:
namely, shaving the hair from the upper part of the head,
in a circular form, so as to leave only an outer ring. The
missionaries have tried to persuade the people to change this
428 CHARLES DARWIN
habit; but it is the fashion, and that is a sufficient answer
at Tahiti, as well as at Paris. I was much disappointed in
the personal appearance of the women: they are far inferior
in every respect to the men. The custom of wearing a white
or scarlet flower in the back of the head, or through a small
hole in each ear, is pretty. A crown of woven cocoa-nut
leaves is also worn as a shade for the eyes. The women
appear to be in greater want of some becoming costume even
than the men.
Nearly all the natives understand a little English — that is,
they know the names of common things; and by the aid of
this, together with signs, a lame sort of conversation could
be carried on. In returning in the evening to the boat, we
stopped to witness a very pretty scene. Numbers of chil-
dren were playing on the beach, and had lighted bonfires
which illumined the placid sea and surrounding trees ;
others, in circles, were singing Tahitian verses. We seated
ourselves on the sand, and joined their party. The songs
were impromptu, and I believe related to our arrival: one
little girl sang a line, which the rest took up in parts, form-
ing a very pretty chorus. The whole scene made us une-
quivocally aware that we were seated on the shores of an
island in the far-famed South Sea.
iyth. — This day is reckoned in the log-book as Tuesday
the 17th, instead of Monday the 16th, owing to our, so far,
successful chase of the sun. Before breakfast the ship was
hemmed in by a flotilla of canoes; and when the natives
were allowed to come on board, I suppose there could not
have been less than two hundred. It was the opinion of
every one that it would have been difficult to have picked out
an equal number from any other nation, who would have
given so little trouble. Everybody brought something for
sale : shells were the main articles of trade. The Tahitians
now fully understand the value of money, and prefer it to
old clothes or other articles. The various coins, however, of
English and Spanish denomination puzzle them, and they
never seemed to think the small silver quite secure until
changed into dollars. Some of the chiefs have accumulated
considerable sums of money. One chief, not long since,
offered 800 dollars (about 160/. sterling) for a small vessel;
THE VOYAGE OF THE BEAGLE 429
and frequently they purchase whale-boats and horses at the
rate of from 50 to 100 dollars.
After breakfast I went on shore, and ascended the nearest
slope to a height of between two and three thousand feet.
The outer mountains are smooth and conical, but steep ; and
the old volcanic rocks, of which they are formed, have been
cut through by many profound ravines, diverging from the
central broken parts of the island to the coast. Having
crossed the narrow low girt of inhabited and fertile land,
I followed a smooth steep ridge between two of the deep
ravines. The vegetation was singular, consisting almost
exclusively of small dwarf ferns, mingled higher up, with
coarse grass; it was not very dissimilar from that on some
of the Welsh hills, and this so close above the orchard of
tropical plants on the coast was very surprising. At the
highest point, which I reached, trees again appeared. Of
the three zones of comparative luxuriance, the lower one
owes its moisture, and therefore fertility, to its flatness ; for,
being scarcely raised above the level of the sea, the water
from the higher land drains away slowly. The intermediate
zone does not, like the upper one, reach into a damp and
cloudy atmospher.e, and therefore remains sterile. The
woods in the upper zone are very pretty, tree-ferns replacing
the cocoa-nuts on the coast. It must not, however, be
supposed that these woods at all equal in splendour the
forests of Brazil. The vast numbers of productions, which
characterize a continent, cannot be expected to occur in
an island.
From the highest point which I attained, there was a good
view of the distant island of Eimeo, dependent on the same
sovereign with Tahiti. On the lofty and broken pinnacles,
white massive clouds were piled up, which formed an island
in the blue sky, as Eimeo itself did in the blue ocean. The
island, with the exception of one small gateway, is completely
encircled by a reef. At this distance, a narrow but well-
defined brilliantly white line was alone visible, where the
waves first encountered the wall of coral. The mountains
rose abruptly out of the glassy expanse of the lagoon, in-
cluded within this narrow white line, outside which the heav-
ing waters of the ocean were dark-coloured. The view was
430 CHARLES DARWIN
striking: it may aptly be compared to a framed engraving,
where the frame represents the breakers, the marginal paper
the smooth lagoon, and the drawing the island itself. When
in the evening I descended from the mountain, a man, whom
I had pleased with a trifling gift, met me, bringing with him
hot roasted bananas, a pine-apple, and cocoa-nuts. After
walking under a burning sun, I do not know anything more
delicious than the milk of a young cocoa-nut. Pine-apples
are here so abundant that the people eat them in the same
wasteful manner as we might turnips. They are of an excel-
lent flavor — perhaps even better than those cultivated in
England; and this I believe is the highest compliment which
can be paid to any fruit. Before going on board, Mr. Wilson
interpreted for me to the Tahitian who had paid me so adroit
an attention, that I wanted him and another man to accom-
pany me on a short excursion into the mountains.
18th. — In the morning I came on shore early, bringing
with me some provisions in a bag, and two blankets for my-
self and servant. These were lashed to each end of a long
pole, which was alternately carried by my Tahitian com-
panions on their shoulders. These men are accustomed thus
to carry, for a whole day, as much as fifty pounds at each
end of their poles. I told my guides to provide themselves
with food and clothing; but they said that there was plenty
of food in the mountains, and for clothing, that their skins
were sufficient. Our line of march was the valley of Tia-
auru, down which a river flows into the sea by Point Venus.
This is one of the principal streams in the island, and its
source lies at the base of the loftiest central pinnacles,
which rise to a height of about 7000 feet. The whole island
is so mountainous that the only way to penetrate into the
interior is to follow up the valleys. Our road, at first, lay
through woods which bordered each side of the river ; and
the glimpses of the lofty central peaks, seen as through an
avenue, with here and there a waving cocoa-nut tree on one
side, were extremely picturesque. The valley soon began to
narrow, and the sides to grow lofty and more precipitous.
After having walked between three and four hours, we
found the width of the ravine scarcely exceeded that of the
bed of the stream. On each hand the walls were nearly ver-
THE VOYAGE OF THE BEAGLE 431
tical; yet from the soft nature of the volcanic strata, trees
and a rank vegetation sprung from every projecting lecige.
These precipices must have been some thousand feet high;
and the whole formed a mountain gorge far more magnifi-
cent than anything which I had ever before beheld. Until
the midday sun stood vertically over the ravine, the air felt
cool and damp, but now it became very sultry. Shaded by a
ledge of rock, beneath a facade of columnar lava, we ate our
dinner. My guides had already procured a dish of small
fish and fresh-water prawns. They carried with them a
small net stretched on a hoop; and where the water was
deep and in eddies, they dived, and like otters, with their
eyes open followed the fish into holes and corners, and thus
caught them.
The Tahitians have the dexterity of amphibious animals
in the water. An anecdote mentioned by Ellis shows how
much they feel at home in this element. When a horse was
landing for Pomarre in 1817, the slings broke, and it fell
into the water; immediately the natives jumped overboard,
and by their cries and vain efforts at assistance almost
drowned it. As soon, however, as it reached the shore, the
whole population took to flight, and tried to hide themselves
from the man-carrying pig, as they christened the horse.
A little higher up, the river divided itself into three little
streams. The two northern ones were impracticable, owing
to a succession of waterfalls which descended from the
jagged summit of the highest mountain; the other to all
appearance was equally inaccessible, but we managed to as-
cend it by a most extraordinary road. The sides of the
valley were here nearly precipitous; but, as frequently hap-
pens with stratified rocks, small ledges projected, which were
thickly covered by wild bananas, lilaceous plants, and other
luxuriant productions of the tropics. The Tahitians, by
climbing amongst these ledges, searching for fruit, had dis-
covered a track by which the whole precipice could be scaled.
The first ascent from the valley was very dangerous; for it
was necessary to pass a steeply inclined face of naked rock,
by the aid of ropes which we brought with us. How any
person discovered that this formidable spot was the only
point where the side of the mountain was practicable, I can-
432 CHARLES DARWIN
not imagine. We then cautiously walked along one of the
ledges till we came to one of the three streams. This ledge
formed a flat spot, above which a beautiful cascade, some
hundred feet in height, poured down its waters, and beneath,
another high cascade fell into the main stream in the val-
ley below. From this cool and shady recess we made a
circuit to avoid the overhanging waterfall. As before, we
followed little projecting ledges, the danger being partly
concealed by the thickness of the vegetation. In passing
from one of the ledges to another, there was a vertical wall
of rock. One of the Tahitians, a fine active man, placed
the trunk of a tree against this, climbed up it, and then by
the aid of crevices reached the summit. He fixed the ropes
to a projecting point, and lowered them for our dog and
luggage, and then we clambered up ourselves. Beneath the
ledge on which the dead tree was placed, the precipice must
have been five or six hundred feet deep; and if the abyss
had not been partly concealed by the overhanging ferns and
lilies my head would have turned giddy, and nothing should
have induced me to have attempted it. We continued to
ascend, sometimes along ledges, and sometimes along knife-
edged ridges, having on each hand profound ravines. In
the Cordillera I have seen mountains on a far grander
scale, but for abruptness, nothing at all comparable with this.
In the evening we reached a flat little spot on the banks
of the same stream, which we had continued to follow, and
which descends in a chain of waterfalls : here we bivouacked
for the night. On each side of the ravine there were great
beds of the mountain-banana, covered with ripe fruit. Many
of these plants were from twenty to twenty-five feet high,
and from three to four in circumference. By the aid of
strips of bark for rope, the stems of bamboos for rafters,
and the large leaf of the banana for a thatch, the Tahitians
in a few minutes built us an excellent house; and with
withered leaves made a soft bed.
They then proceeded to make a fire, and cook our evening
meal. A light was procured, by rubbing a blunt pointed
stick in a groove made in another, as if with intention of
deepening it, until by the friction the dust became ignited.
A peculiarly white and very light wood (the Hibiscus tilia-
THE VOYAGE OF THE BEAGLE 433
ceus) is alone used for this purpose: it is the same which
serves for poles to carry any burden, and for the floating
out-riggers to their canoes. The fire was produced in a few
seconds: but to a person who does not understand the art,
it requires, as I found, the greatest exertion; but at last, to
my great pride, I succeeded in igniting the dust. The
Gaucho in the Pampas uses a different method: taking an
elastic stick about eighteen inches long, he presses one end
on his breast, and the other pointed end into a hole in a piece
of wood, and then rapidly turns the curved part, like a car-
penter's centre-bit. The Tahitians having made a small fire
of sticks, placed a score of stones, of about the size of
cricket-balls, on the burning wood. In about ten minutes the
sticks were consumed, and the stones hot. They had previ-
ously folded up in small parcels of leaves, pieces of beef,
fish, ripe and unripe bananas, and the tops of the wild arum.
These green parcels were laid in a layer between two layers
of the hot stones, and the whole then covered up with
earth, so that no smoke or steam could escape. In about
a quarter of an hour, the whole was most deliciously cooked.
The choice green parcels were now laid on a cloth of
banana leaves, arid with a cocoa-nut shell we drank the
cool water of the running stream; and thus we enjoyed our
rustic meal.
I could not look on the surrounding plants without ad-
miration. On every side were forests of banana; the fruit
of which, though serving for food in various ways, lay in
heaps decaying on the ground. In front of us there was an
extensive brake of wild sugar-cane; and the stream was
shaded by the dark green knotted stem of the Ava, — so fa-
mous in former days for its powerful intoxicating effects. I
chewed a piece, and found that it had an acrid and unpleasant
taste, which would have induced any one at once to
have pronounced it poisonous. Thanks to the missionaries,
this plant now thrives only in these deep ravines, innocuous to
every one. Close by I saw the wild arum, the roots of which,
when well baked, are good to eat, and the young leaves
better than spinach. There was the wild yam, and a liliaceous
plant called Ti, which grows in abundance, and has a soft
brown root, in shape and size like a huge log of wood: this
434 CHARLES DARWIN
served us for dessert, for it is as sweet as treacle, and with
a pleasant taste. There were, moreover, several other wild
fruits, and useful vegetables. The little stream, besides its
cool water, produced eels, and cray-fish. I did indeed admire
this scene, when I compared it with an uncultivated one in
the temperate zones. I felt the force of the remark, that
man, at least savage man, with his reasoning powers only
partly developed, is the child of the tropics.
As the evening drew to a close, I strolled beneath the
gloomy shade of the bananas up the course of the stream.
My walk was soon brought to a close, by coming to a water-
fall between two and three hundred feet high; and again
above this there was another. I mention all these waterfalls
in this one brook, to give a general idea of the inclination
of the land. In the little recess where the water fell, it did
not appear that a breath of wind had ever blown. The thin
edges of the great leaves of the banana, damp with spray,
were unbroken, instead of being, as is so generally the case,
split into a thousand shreds. From our position, almost sus-
pended on the mountain side, there were glimpses into the
depths of the neighbouring valleys; and the lofty points of
the central mountains, towering up within sixty degrees of
the zenith, hid half the evening sky. Thus seated, it was
a sublime spectacle to watch the shades of night gradually
obscuring the last and highest pinnacles.
Before we laid ourselves down to sleep, the elder Tahitian
fell on his knees, and with closed eyes repeated a long
prayer in his native tongue. He prayed as a Christian should
do, with fitting reverence, and without the fear of ridicule
or any ostentation of piety. At our meals neither of the men
would taste food, without saying beforehand a short grace.
Those travellers who think that a Tahitian prays only when
the eyes of the missionary are fixed on him, should have
slept with us that night on the mountain-side. Before morn-
ing it rained very heavily; but the good thatch of banana-
leaves kept us dry.
November ipth. — At daylight my friends, after their
morning prayer, prepared an excellent breakfast in the same
manner as in the evening. They themselves certainly par-
took of it largely; indeed I never saw any men eat near so
THE VOYAGE OF THE BEAGLE 435
much. I suppose such enormously capacious stomachs must
be the effect of a large part of their diet consisting of fruit
and vegetables, which contain, in a given bulk, a compara-
tively small portion of nutriment. Unwittingly, I was the
tneans of my companions breaking, as I afterwards learned,
one of their own laws, and resolutions: I took with me a
flask of spirits, which they could not refuse to partake of;
but as often as they drank a little, they put their fingers
before their mouths, and uttered the word "Missionary."
About two years ago, although the use of the ava was pre-
vented, drunkenness from the introduction of spirits became
very prevalent. The missionaries prevailed on a few good
men, who saw that their country was rapidly going to ruin,
to join with them in a Temperance Society. From good
sense or shame, all the chiefs and the queen were at last per-
suaded to join. Immediately a law was passed, that no
spirits should be allowed to be introduced into the island,
and that he who sold and he who bought the forbidden
article should be punished by a fine. With remarkable jus-
tice, a certain period was allowed for stock in hand to be
sold, before the law came into effect. But when it did, a
general search was made, in which even the houses of the
missionaries were not exempted, and all the ava (as the
natives call all ardent spirits) was poured on the ground.
When one reflects on the effect of intemperance on the
aborigines of the two Americas, I think it will be acknowl-
edged that every well-wisher of Tahiti owes no common debt
of gratitude to the missionaries. As long as the little island
of St. Helena remained under the government of the East
India Company, spirits, owing to the great injury they had
produced, were not allowed to be imported; but wine was
supplied from the Cape of Good Hope. It is rather a strik-
ing and not very gratifying fact, that in the same year
that spirits were allowed to be sold in Helena, their use was
banished from Tahiti by the free will of the people.
After breakfast we proceeded on our journey. As my ob-
ject was merely to see a little of the interior scenery, we
returned by another track, which descended into the main
valley lower down. For some distance we wound, by a most
intricate path, along the side of the mountain which formed
436 CHARLES DARWIN
the valley. In the less precipitous parts we passed through
extensive groves of the wild banana. The Tahitians, with
their naked, tattooed bodies, their heads ornamented with
flowers, and seen in the dark shade of these groves, would
have formed a fine picture of man inhabiting some primeval
land. In our descent we followed the line of ridges; these
were exceedingly narrow, and for considerable lengths steep
as a ladder; but all clothed with vegetation. The extreme
care necessary in poising each step rendered the walk fa-
tiguing. I did not cease to wonder at these ravines and
precipices: when viewing the country from one of the knife-
edged ridges, the point of support was so small, that the
effect was nearly the same as it must be from a balloon. In
this descent we had occasion to use the ropes only once, at
the point where we entered the main valley. We slept under
the same ledge of rock where we had dined the day before :
the night was fine, but from the depth and narrowness of the
gorge, profoundly dark.
Before actually seeing this country, I found it difficult
to understand two facts mentioned by Ellis; namely, that
after the murderous battles of former times, the survivors
on the conquered side retired into the mountains, where a
handful of men could resist a multitude. Certainly half
a dozen men, at the spot where the Tahitian reared the old
tree, could easily have repulsed thousands. Secondly, that
after the introduction of Christianity, there were wild men
who lived in the mountains, and whose retreats were un-
known to the more civilized inhabitants.
November 20th. — In the morning we started early, and
reached Matavai at noon. On the read we met a large party
of noble athletic men, going for wild bananas. I found that
the ship, on account of the difficulty in watering, had moved
to the harbour of Papawa, to which place I immediately
walked. This is a very pretty spot. The cove is surrounded
by reefs, and the water as smooth as in a lake. The
cultivated ground, with its beautiful productions, inter-
spersed with cottages, comes close down to the water's edge.
From the varying accounts which I had read before reach-
ing these islands, I was very anxious to form, from my own
observation, a judgment of their moral state, — although such
THE VOYAGE OF THE BEAGLE 437
judgment would necessarily be very imperfect. First im-
pressions at all times very much depend on one's previously
acquired ideas. My notions were drawn from Ellis's " Poly-
nesian Researches " — an admirable and most interesting
work, but naturally looking at everything under a favourable
point of view; from Beechey's Voyage; and from that of
Kotzebue, which is strongly adverse to the whole missionary
system. He who compares these three accounts will, I think,
form a tolerably accurate conception of the present state of
Tahiti. One of my impressions, which I took from the two
last authorities, was decidedly incorrect; viz., that the Ta-
hitians had become a gloomy race, and lived in fear of the
missionaries. Of the latter feeling I saw no trace, unless,
indeed, fear and respect be confounded under one name.
Instead of discontent being a common feeling, it would be
difficult in Europe to pick out of a crowd half so many merry
and happy faces. The prohibition of the flute and dancing
is inveighed against as wrong and foolish; — the more than
presbyterian manner of keeping the sabbath is looked at in
a similar light. On these points I will not pretend to offer
any opinion to men who have resided as many years as I
was days on the island.
On the whole, it appears to me that the morality and
religion of the inhabitants are highly creditable. There arc
many who attack, even more acrimoniously than Kotzebue,
both the missionaries, their system, and the effects produced
by it Such reasoners never compare the present state with
that of the island only twenty years ago ; nor even with that
of Europe at this day; but they compare it with the high
standard of Gospel perfection. They expect the missionaries
to effect that which the Apostles themselves failed to do.
Inasmuch as the condition of the people falls short of
this high standard, blame is attached to the missionary, in-
stead of credit for that which he has effected. They forget,
or will not remember, that human sacrifices, and the power
of an idolatrous priesthood — a system of profligacy unparal-
leled in any other part of the world — infanticide a consequence
of that system — bloody wars, where the conquerors spared
neither women nor children — that all these have been abol-
ished; and that dishonesty, intemperance, and licentiousness
438 CHARLES DARWIN
have been greatly reduced by the introduction of Christianity.
In a voyager to forget these things is base ingratitude; for
should he chance to be at the point of shipwreck on some
unknown coast, he will most devoutly pray that the lesson of
the missionary may have extended thus far.
In point of morality, the virtue of the women, it has been
often said, is most open to exception. But before they are
blamed too severely, it will be well distinctly to call to mind
the scenes described by Captain Cook and Mr. Banks, in
which the grandmothers and mothers of the present race
played a part. Those who are most severe, should consider
how much of the morality of the women in Europe is owing
to the system early impressed by mothers on their daughters,
and how much in each individual case to the precepts of re-
ligion. But it is useless to argue against such reasoners; — I
believe that, disappointed in not finding the field of licen-
tiousness quite so open as formerly, they will not give credit
to a morality which they do not wish to practise, or to a
religion which they undervalue, if not despise.
Sunday, 22nd. — The harbour of Papiete, where the queen
resides, may be considered as the capital of the island: it is
also the seat of government, and the chief resort of shipping.
Captain Fitz Roy took a party there this day to hear divine
service, first in the Tahitian language, and afterwards in our
own. Mr. Pritchard, the leading missionary in the island,
performed the service. The chapel consisted of a large airy
framework of wood; and it was filled to excess by tidy, clean
people, of all ages and both sexes. I was rather disappointed
in the apparent degree of attention; but I believe my ex-
pectations were raised too high. At all events the appear-
ance was quite equal to that in a country church in England.
The singing of the hymns was decidedly very pleasing, but
the language from the pulpit, although fluently delivered, did
not sound well : a constant repetition of words, like " tata
ta, mata mai," rendered it monotonous. After English serv-
ice, a party returned on foot to Matavai. It was a pleasant
walk, sometimes along the sea-beach and sometimes under
the shade of the many beautiful trees.
About two years ago, a small vessel under English colours
was plundered by some of the inhabitants of the Low Islands,
THE VOYAGE OF THE BEAGLE 439
which were then under the dominion of the Queen of Tahiti.
It was believed that the perpetrators were instigated to this
act by some indiscreet laws issued by her majesty. The
British government demanded compensation; which was ac-
ceded to, and the sum of nearly three thousand dollars was
agreed to be paid on the first of last September. The Com-
modore at Lima ordered Captain Fitz Roy to inquire con-
cerning this debt, and to demand satisfaction if it were not
paid. Captain Fitz Roy accordingly requested an interview
with the Queen Pomarre, since famous from the ill-treatment
she had received from the French; and a parliament was
held to consider the question, at which all the principal chiefs
of the island and the queen were assembled. I will not at-
tempt to describe what took place, after the interesting ac-
count given by Captain Fitz Roy. The money, it appeared,
had not been paid; perhaps the alleged reasons were rather
equivocal; but otherwise I cannot sufficiently express our
general surprise at the extreme good sense, the reasoning
powers, moderation, candour, and prompt resolution, which
were displayed on all sides. I believe we all left the meeting
with a very different opinion of the Tahitians, from what we
entertained when we entered. The chiefs and people re-
solved to subscribe and complete the sum which was want-
ing; Captain Fitz Roy urged that it was hard that their pri-
vate property should be sacrificed for the crimes of distant
islanders. They replied, that they were grateful for his con-
sideration, but that Pomarre was their Queen, and that they
were determined to help her in this her difficulty. This reso-
lution and its prompt execution, for a book was opened
early the next morning, made a perfect conclusion to this
very remarkable scene of loyalty and good feeling.
After the main discussion was ended, several of the chiefs
took the opportunity of asking Captain Fitz Roy many in-
telligent questions on international customs and laws, relat-
ing to the treatment of ships and foreigners. On some
points, as soon as the decision was made, the law was issued
verbally on the spot. This Tahitian parliament lasted for
several hours; and when it was over Captain Fitz Roy in-
vited Queen Pomarre to pay the Beagle a visit.
November 25th. — In the evening four boats were sent for
440 CHARLES DARWIN
her majesty; the ship was dressed with flags, and the yards
manned on her coming on board. She was accompanied by
most of the chiefs. The behaviour of all was very proper:
they begged for nothing, and seemed much pleased with Cap-
tain Fitz Roy's presents. The queen is a large awkward
woman, without any beauty, grace or dignity. She has only
one royal attribute : a perfect immovability of expression
under all circumstances, and that rather a sullen one. The
rockets were most admired; and a deep " Oh ! " could be
heard from the shore, all round the dark bay, after each ex-
plosion. The sailors' songs were also much admired; and
the queen said she thought that one of the most boisterous
ones certainly could not be a hymn ! The royal party did
not return on shore till past midnight.
26th. — In the evening, with a gentle land-breeze, a course
was steered for New Zealand; and as the sun set, we had a
farewell view of the mountains of Tahiti — the island to which
every voyager has offered up his tribute of admiration.
December igth. — In the evening we saw in the distance
New Zealand. We may now consider that we have nearly
crossed the Pacific. It is necessary to sail over this great
ocean to comprehend its immensity. Moving quickly on-
wards for weeks together, we meet with nothing but the
same blue, profoundly deep, ocean. Even within the archi-
pelagoes, the islands are mere specks, and far distant one
from the other. Accustomed to look at maps drawn on a
small scale, where dots, shading, and names are crowded
together, we do not rightly judge how infinitely small the
proportion of dry land is to water of this vast expanse.
The meridian of the Antipodes has likewise been passed ; and
now every league, it made us happy to think, was one league
nearer to England. These Antipodes call to one's mind old
recollections of childish doubt and wonder. Only the other
day I looked forward to this airy barrier as a definite point
in our voyage homewards; but now I find it, and all such
resting-places for the imagination, are like shadows, which
a man moving onwards cannot catch. A gale of wind last-
ing for some days, has lately given us full leisure to measure
the future stages in our homeward voyage, and to wish
most earnestly for its termination.
THE VOYAGE OF THE BEAGLE 441
December 21st. — Early in the morning we entered the Bay
of Islands, and being becalmed for some hours near the
mouth, we did not reach the anchorage till the middle of the
day. The country is hilly, with a smooth outline, and is
deeply intersected by numerous arms of the sea extending
from the bay. The surface appears from a distance as if
clothed with coarse pasture, but this in truth is nothing but
fern. On the more distant hills, as well as in parts of the
valleys, there is a good deal of woodland. The general tint
of the landscape is not a bright green; and it resembles the
country a short distance to the south of Concepcion in Chile.
In several parts of the bay, little villages of square tidy-look-
ing houses are scattered close down to the water's edge.
Three whaling-ships were lying at anchor, and a canoe every
now and then crossed from shore to shore; with these
exceptions, an air of extreme quietness reigned over the
whole district. Only a single canoe came alongside. This,
and the aspect of the whole scene, afforded a remarkable,
and not very pleasing contrast, with our joyful and boisterous
welcome at Tahiti.
In the afternoon we went on shore to one of the larger
groups of houses, which yet hardly deserves the title of a
village. Its name is Pahia : it is the residence of the mis-
sionaries; and there are no native residents except servants
and labourers. In the vicinity of the Bay of Islands, the
number of Englishmen, including their families, amounts to
between two and three hundred. All the cottages, many of
which are white-washed and look very neat, are the property
of the English. The hovels of the natives are so diminutive
and paltry, that they can scarcely be perceived from a dis-
tance. At Pahia, it was quite pleasing to behold the En-
glish flowers in the gardens before the houses; there were
roses of several kinds, honeysuckle, jasmine, stocks, and
whole hedges of sweetbrier.
December ?2nd. — In the morning I went out walking; but
I soon found that the country was very impracticable. All
the hills are thickly covered with tall fern, together with
a low bush which grows like a cypress; and very little
ground has been cleared or cultivated. I then tried the
sea-beach; but proceeding towards either hand, my walk
442 CHARLES DARWIN
was soon stopped by salt-water creeks and deep brooks. The
communication between the inhabitants of the different
parts of the bay, is (as in Chiloe) almost entirely kept up
by boats. I was surprised to find that almost every hill which
I ascended, had been at some former time more or less
fortified. The summits were cut into steps or successive
terraces, and frequently they had been protected by deep
trenches. I afterwards observed that the principal hills in-
land in like manner showed an artificial outline. These are
the Pas, so frequently mentioned by Captain Cook under the
name of " hippah ; " the difference of sound being owing to
the prefixed article.
That the Pas had formerly been much used, was evident
from the piles of shells, and the pits in which, as I was
informed, sweet potatoes used to be kept as a reserve. As
there was no water on these hills, the defenders could never
have anticipated a long siege, but only a hurried attack for
plunder, against which the successive terraces would have
afforded good protection. The general introduction of fire-
arms has changed the whole system of warfare; and an ex-
posed situation on the top of a hill is now worse than useless.
The Pas in consequence are, at the present day, always built
on a level piece of ground. They consist of a double stockade
of thick and tall posts, placed in a zigzag line, so that every
part can be flanked. Within the stockade a mound of earth is
thrown up, behind which the defenders can rest in safety, or
use their fire-arms over it. On the level of the ground
little archways sometimes pass through this breastwork,
by which means the defenders can crawl out to the stockade
and reconnoitre their enemies. The Rev. W. Williams, who
gave me this account, added, that in one Pas he had noticed
spurs or buttresses projecting on the inner and protected
side of the mound of earth. On asking the chief the use
of them, he replied, that if two or three of his men were
shot, their neighbours would not see the bodies, and so be
discouraged.
These Pas are considered by the New Zealanders as very
perfect means of defence: for the attacking force is never
so well disciplined as to rush in a body to the stockade, cut
it down, and effect their entry. When a tribe goes to war,
THE VOYAGE OF THE BEAGLE 443
the chief cannot order one party to go here and another
there ; but every man fights in the manner which best pleases
himself; and to each separate individual to approach a stock-
ade defended by fire-arms must appear certain death. I
should think a more warlike race of inhabitants could not
be found in any part of the world than the New Zealanders.
Their conduct on first seeing a ship, as described by Captain
Cook, strongly illustrates this: the act of throwing volleys
of stones at so great and novel an object, and their defiance
of " Come on shore and we will kill and eat you all," shows
uncommon boldness. This warlike spirit is evident in many
of their customs, and even in their smallest actions. If a
New Zealander is struck, although but in joke, the blow
must be returned and of this I saw an instance with one
of our officers.
At the present day, from the progress of civilization, there
is much less warfare, except among some of the southern
tribes. I heard a characteristic anecdote of what took place
some time ago in the south. A missionary found a chief and
his tribe in preparation for war; — their muskets clean and
bright, and their ammunition ready. He reasoned long on
the inutility of the war, and the little provocation which
had been given for it. The chief was much shaken in his
resolution, and seemed in doubt: but at length it occurred
to him that a barrel'of his gunpowder was in a bad state, and
that it would not keep much longer. This was brought for-
ward as an unanswerable argument for the necessity of im-
mediately declaring war : the idea of allowing so much good
gunpowder to spoil was not to be thought of; and this set-
tled the point. I was told by the missionaries that in the
life of Shongi, the chief who visited England, the love of
war was the one and lasting spring of every action. The
tribe in which he was a principal chief had at one time been
oppressed by another tribe from the Thames River. A
solemn oath was taken by the men that when their boys
should grow up, and they should be powerful enough, they
would never forget or forgive these injuries. To fulfil this
oath appears to have been Shongi's chief motive for going
to England; and when there it was his sole object. Pres-
ents were valued only as they could be converted into arms ;
444 CHARLES DARWIN
of the arts, those alone interested him which were connected
with the manufacture of arms. When at Sydney, Shongi,
by a strange coincidence, met the hostile chief of the Thames
River at the house of Mr. Marsden : their conduct was civil
to each other; but Shongi told him that when again in New
Zealand he would never cease to carry war into his country.
The challenge was accepted; and Shongi on his return ful-
filled the threat to the utmost letter. The tribe on the
Thames River was utterly overthrown, and the chief to
whom the challenge had been given was himself killed.
Shongi, although harbouring such deep feelings of hatred
and revenge, is described as having been a good-natured
person.
In the evening I went with Captain Fitz Roy and Mr.
Baker, one of the missionaries, to pay a visit to Kororadika :
we wandered about the village, and saw and conversed with
many of the people, both men, women, and children. Look-
ing at the New Zealander, one naturally compares him with
the Tahitian ; both belonging to the same family of mankind.
The comparison, however, tells heavily against the New
Zealander. He may, perhaps be superior in energy, but
in every other respect his character is of a much lower
order. One glance at their respective expressions, brings
conviction to the mind that one is a savage, the other a
civilized man. It would be vain to seek in the whole of
New Zealand a person with the face and mien of the old
Tahitian chief Utamme. No doubt the extraordinary manner
in which tattooing is here practised, gives a disagreeable
expression to their countenances. The complicated but sym-
metrical figures covering the whole face, puzzle and mislead
an unaccustomed eye : it is moreover probable, that the deep
incisions, by destroying the play of the superficial muscles,
give an air of rigid inflexibility. But, besides this, there is
a twinkling in the eye, which cannot indicate anything but
cunning and ferocity. Their figures are tall and bulky; but
not comparable in elegance with those of the working-
classes in Tahiti.
But their persons and houses are filthily dirty and offen-
sive: the idea of washing either their bodies or their clothes
never seems to enter their heads. I saw a chief, who was
THE VOYAGE OF THE BEAGLE 445
wearing a shirt black and matted with filth, and when asked
how it came to be so dirty, he replied, with surprise, " Do
not you see it is an old one? " Some of the men have shirts ;
but the common dress is one or two large blankets, generally
black with dirt, which are thrown over their shoulders in a
very inconvenient and awkward fashion. A few of the prin-
cipal chiefs have decent suits of English clothes; but these
are only worn on great occasions.
December 23rd. — At a place called Waimate, about fifteen
miles from the Bay of Islands, and midway between the
eastern and western coasts, the missionaries have purchased
some land for agricultural purposes. I had been introduced
to the Rev. W. Williams, who, upon my expressing a wish,
invited me to pay him a visit there. Mr. Bushby, the British
resident, offered to take me in his boat by a creek, where I
should see a pretty waterfall, and by which means my
walk would be shortened. He likewise procured for me a
guide.
Upon asking a neighbouring chief to recommend a man, the
chief himself offered to go; but his ignorance of the value
of money was so complete, that at first he asked how many
pounds I would give him, but afterwards was well contented
with two dollars. When I showed the chief a very small
bundle, which I wanted carried, it became absolutely neces-
sary for him to take a slave. These feelings of pride are
beginning to wear away ; but formerly a leading man would
sooner have died, than undergone the indignity of carrying
the smallest burden. My companion was a light active man,
dressed in a dirty blanket, and with his face completely
tattooed. He had formerly been a great warrior. He ap-
peared to be on very cordial terms with Mr. Bushby ; but at
various times they had quarrelled violently. Mr. Bushby
remarked that a little quiet irony would frequently silence
any one of these natives in their most blustering moments.
This chief has come and harangued Mr. Bushby in a hec-
toring manner, saying, " great chief, a great man, a friend
of mine, has come to pay me a visit — you must give him
something good to eat, some fine presents, etc." Mr. Bushby
has allowed him to finish his discourse, and then has quietly
replied by some answer such as, " What else shall your slave
446 CHARLES DARWIN
do for you ? " The man would then instantly, with a very
comical expression, cease his braggadocio.
Some time ago, Mr. Bushby suffered a far more serious
attack. A chief and a party of men tried to break into his
house in the middle of the night, and not finding this so easy,
commenced a brisk firing with their muskets. Mr. Bushby
was slightly wounded, but the party was at length driven
away. Shortly afterwards it was discovered who was the
aggressor ; and a general meeting of the chiefs was convened
to consider the case. It was considered by the New Zealand-
ers as very atrocious, inasmuch as it was a night attack, and
that Mrs. Bushby was lying ill in the house : this latter cir-
cumstance, much to their honour, being considered in all
cases as a protection. The chiefs agreed to confiscate the
land of the aggressor to the King of England. The whole
proceeding, however, in thus trying and punishing a chief
was entirely without precedent. The aggressor, moreover,
lost caste in the estimation of his equals and this was con-
sidered by the British as of more consequence than the con-
fiscation of his land.
As the boat was shoving off, a second chief stepped into
her, who only wanted the amusement of the passage up and
down the creek. I never saw a more horrid and ferocious
expression than this man had. It immediately struck me
I had somewhere seen his likeness: it will be found in
Retzch's outlines to Schiller's ballad of Fridolin, where two
men are pushing Robert into the burning iron furnace. It
is the man who has his arm on Robert's breast. Physiog-
nomy here spoke the truth; this chief had been a notorious
murderer, and was an arrant coward to boot. At the point
where the boat landed, Mr. Bushby accompanied me a few
hundred yards on the road: I could not help admiring the
cool impudence of the hoary old villain, whom we left lying
in the boat, when he shouted to Mr. Bushby, " Do not you
stay long, I shall be tired of waiting here."
We now commenced our walk. The road lay along a
well beaten path, bordered on each side by the tall fern,
which covers the whole country. After travelling some
miles, we came to a little country village, where a few hovels
were collected together, and some patches of ground culti-
THE VOYAGE OF THE BEAGLE 447
vated with potatoes. The introduction of the potato has
been the most essential benefit to the island ; it is now much
more used than any native vegetable. New Zealand is
favoured by one great natural advantage; namely, that the
inhabitants can never perish from famine. The whole
country abounds with fern: and the roots of this plant, if
not very palatable, yet contain much nutriment. A native
can always subsist on these, and on the shell-fish, which are
abundant on all parts of the sea-coast. The villages are
chiefly conspicuous by the platforms which are raised on
four posts ten or twelve feet above the ground, and on
which the produce of the fields is kept secure from all
accidents.
On coming near one of the huts I was much amused by
seeing in due form the ceremony of rubbing, or, as it ought
to be called, pressing noses. The women, on our first ap-
proach, began uttering something in a most dolorous voice;
they then squatted themselves down and held up their faces ;
my companion standing over them, one after another, placed
the bridge of his nose at right angles to theirs, and com-
menced pressing. This lasted rather longer than a cordial
shake of the hand with us; and as we vary the force of the
grasp of the hand in shaking, so do they in pressing. Dur-
ing the process they uttered comfortable little grunts, very
much in the same manner as two pigs do, when rubbing
against each other. I noticed that the slave would press
noses with any one he met, indifferently either before or
after his master the chief. Although among the savages, the
chief has absolute power of life and death over his slave,
yet there is an entire absence of ceremony between them.
Mr. Burchell has remarked the same thing in Southern Af-
rica, with the rude Bachapins. Where civilization has
arrived at a certain point, complex formalities soon arise
between the different grades of society: thus at Tahiti all
were formerly obliged to uncover themselves as low as the
waist in presence of the king.
The ceremony of pressing noses having been duly com-
pleted with all present, we seated ourselves in a circle in the
front of one of the hovels, and rested there half-an-hour.
All the hovels have nearly the same form and dimensions,
448 CHARLES DARWIN
and all agree in being filthily dirty. They resemble a cow-
shed with one end open, but having a partition a little way
within, with a square hole in it, making a small gloomy
chamber. In this the inhabitants keep all their property,
and when the weather is cold they sleep there. They eat,
however, and pass their time in the open part in front. My
guides having finished their pipes, we continued our walk.
The path led through the same undulating country, the whole
uniformly clothed as before with fern. On our right hand
we had a serpentine river, the banks of which were fringed
with trees, and here and there on the hill sides there was a
clump of wood. The whole scene, in spite of its green col-
our, had rather a desolate aspect. The sight of so much fern
impresses the mind with an idea of sterility: this, however,
is not correct ; for wherever the fern grows thick and breast-
high, the land by tillage becomes productive. Some of the
residents think that all this extensive open country originally
was covered with forests, and that it has been cleared by fire.
It is said, that by digging in the barest spots, lumps of the
kind of resin which flows from the kauri pine are frequently
found. The natives had an evident motive in clearing the
country; for the fern, formerly a staple article of food,
flourishes only in the open cleared tracks. The almost entire
absence of associated grasses, which forms so remarkable a
feature in the vegetation of this island, may perhaps be
accounted for by the land having been aboriginally covered
with forest-trees.
The soil is volcanic; in several parts we passed over
shaggy lavas, and craters could clearly be distinguished on
several of the neighbouring hills. Although the scenery is
nowhere beautiful, and only occasionally pretty, I enjoyed
my walk. I should have enjoyed it more, if my companion,
the chief, had not possessed extraordinary conversational
powers. I knew only three words : " good," " bad," and
" yes : " and with these I answered all his remarks, without
of course having understood one word he said. This, how-
ever, was quite sufficient : I was a good listener, an agreeable
person, and he never ceased talking to me.
At length we reached Waimate. After having passed over
so many miles of an uninhabited useless country, the sudden
THE VOYAGE OF THE BEAGLE 449
appearance of an English farm-house, and its well-dressed
fields, placed there as if by an enchanter's wand, was exceed-
ingly pleasant. Mr. Williams not being at home, I received
in Mr. Davies's house a cordial welcome. After drinking tea
with his family party, we took a stroll about the farm. At
Waimate there are three large houses, where the missionary
gentlemen, Messrs. Williams, Davies, and Clarke, reside;
and near them are the huts of the native labourers. On an
adjoining slope, fine crops of barley and wheat were standing
in full ear ; and in another part, fields of potatoes and clover.
But I cannot attempt to describe all I saw ; there were large
gardens, with every fruit and vegetable which England pro-
duces; and many belonging to a warmer clime. I may
instance asparagus, kidney beans, cucumbers, rhubarb, apples,
pears, figs, peaches, apricots, grapes, olives, gooseberries,
currants, hops, gorse for fences, and English oaks ; also many
kinds of flowers. Around the farm-yard there were stables,
a thrashing-barn with its winnowing machine, a blacksmith's
forge, and on the ground ploughshares and other tools: in
the middle was that happy mixture of pigs and poultry, lying
comfortably together, as in every English farm-yard. At the
distance of a few hundred yards, where the water of a little
rill had been dammed up into a pool, there was a large and
substantial water-mill.
All this is very surprising, when it is considered that five
years ago nothing but the fern flourished here. Moreover,
native workmanship, taught by the missionaries, has effected
this change; — the lesson of the missionary is the enchanter's
wand. The house had been built, the windows framed, the
fields ploughed, and even the trees grafted, by a New Zea-
lander. At the mill, a New Zealander was seen powdered
white with flower, like his brother miller in England. When
I looked at this whole scene, I thought it admirable. It was
not merely that England was brought vividly before my
mind; yet, as the evening drew to a close, the domestic
sounds, the fields of corn, the distant undulating country
with its trees might well have been mistaken for our father-
land : nor was it the triumphant feeling at seeing what Eng-
lishmen could effect ; but rather the high hopes thus inspired
for the future progress of this fine island.
vol. xxix — o hc
450 CHARLES DARWIN
Several young men, redeemed by the missionaries from
slavery, were employed on the farm. They were dressed in
a shirt, jacket, and trousers, and had a respectable appear-
ance. Judging from one trifling anecdote, I should think
they must be honest. When walking in the fields, a young
labourer came up to Mr. Davies, and gave him a knife and
gimlet, saying that he had found them on the road, and did
not know to whom they belonged ! These young men and
boys appeared very merry and good-humoured. In the even-
ing I saw a party of them at cricket : when I thought of the
austerity of which the missionaries have been accused, I was
amused by observing one of their own sons taking an active
part in the game. A more decided and pleasing change was
manifested in the young women, who acted as servants within
the houses. Their clean, tidy, and healthy appearance, like
that of the dairy-maids in England, formed a wonderful
contrast with the women of the filthy hovels in Kororadika.
The wives of the missionaries tried to persuade them not to
be tattooed; but a famous operator having arrived from the
south, they, said, " We really must just have a few lines on
our lips ; else when we grow old, our lips will shrivel, and we
shall be so very ugly." There is not nearly so much tattooing
as formerly; but as it is a badge of distinction between the
chief and the slave, it will probably long be practised. So
soon does any train of ideas become habitual, that the mis-
sionaries told me that even in their eyes a plain face looked
mean, and not like that of a New Zealand gentleman.
Late in the evening I went to Mr. Williams's house, where
I passed the night. I found there a large party of children,
collected together for Christmas Day, and all sitting round
a table at tea. I never saw a nicer or more merry group ; and
to think that this was in the centre of the land of cannibal-
ism, murder, and all atrocious crimes! The cordiality and
happiness so plainly pictured in the faces of the little circle,
appeared equally felt by the older persons of the mission.
December 24th. — In the morning, prayers were read in
the native tongue to the whole family. After breakfast I
rambled about the gardens and farm. This was a market-
day, when the natives of the surrounding hamlets bring their
potatoes, Indian corn, or pigs, to exchange for blankets,
THE VOYAGE OF THE BEAGLE 451
tobacco, and sometimes, through the persuasions of the mis-
sionaries, for soap. Mr. Davies's eldest son, who manages a
farm of his own, is the man of business in the market. The
children of the missionaries, who came while young to the
island, understand the language better than their parents,
and can get anything more readily done by the natives.
A little before noon Messrs. Williams and Davies walked
with me to a part of a neighbouring forest, to show me the
famous kauri pine. I measured one of the noble trees, and
found it thirty-one feet in circumference above the roots.
There was another close by, which I did not see, thirty-three
feet; and I heard of one no less than forty feet. These trees
are remarkable for their smooth cylindrical boles, which run
up to a height of sixty, and even ninety feet, with a nearly
equal diameter, and without a single branch. The crown
of branches at the summit is out of all proportion small to
the trunk; and the leaves are likewise small compared with
the branches. The forest was here almost composed of the
kauri; and the largest trees, from the parallelism of their
sides, stood up like gigantic columns of wood. The timber
of the kauri is the most valuable production of the island;
moreover, a quantity of resin oozes from the bark, which is
sold at a penny a pound to the Americans, but its use was
then unknown. Some of the New Zealand forest must be
impenetrable to an extraordinary degree. Mr. Matthews
informed me that one forest only thirty-four miles in width,
and separating two inhabited districts, had only lately, for
the first time, been crossed. He and another missionary,
each with a party of about fifty men, undertook to open a
road; but it cost more than a fortnight's labour! In
the woods I saw very few birds. With regard to animals,
it is a most remarkable fact, that so large an island, extend-
ing over more than 700 miles in latitude, and in many parts
ninety broad, with varied stations, a fine climate, and land
of all heights, from 14,000 feet downwards, with the excep-
tion of a small rat, did not possess one indigenous animal.
The several species of that gigantic genus of birds, the Dei-
nornis seem here to have replaced mammiferous quadrupeds,
in the same manner as the reptiles still do at the Galapagos
archipelago. It is said that the common Norway rat, in
452 CHARLES DARWIN
the short space of two years, annihilated in this northern
end of the island, the New Zealand species. In many places
I noticed several sorts of weeds, which, like the rats, I was
forced to own as countrymen. A leek has overrun whole
districts, and will prove very troublesome, but it was im-
ported as a favour by a French vessel. The common dock
is also widely disseminated, and will, I fear, for ever remain
a proof of the rascality of an Englishman, who sold the seeds
for those of the tobacco plant.
On returning from our pleasant walk to the house, I dined
with Mr. Williams; and then, a horse being lent me, I re-
turned to the Bay of Islands. I took leave of the missionaries
with thankfulness for their kind welcome, and with feel-
ings of high respect for their gentlemanlike, useful, and
upright characters. I think it would be difficult to find
a body of men better adapted for the high office which
they fulfil.
Christmas Day. — In a few more days the fourth year of
our absence from England will be completed. Our first
Christmas Day was spent at Plymouth; the second at St.
Martin's Cove, near Cape Horn; the third at Port Desire,
in Patagonia ; the fourth at anchor in a wild harbour in the
peninsula of Tres Montes; this fifth here; and the next, I
trust in Providence, will be in England. We attended divine
service in the chapel of Pahia; part of the service being
read in English, and part in the native language. Whilst at
New Zealand we did not hear of any recent acts of canni-
balism; but Mr. Stokes found burnt human bones strewed
round a fire-place on a small island near the anchorage ; but
these remains of a comfortable banquet might have been
lying there for several years. It is probable that the moral
state of the people will rapidly improve. Mr. Bushby men-
tioned one pleasing anecdote as a proof of the sincerity of
some, at least, of those who profess Christianity. One of
his young men left him, who had been accustomed to read
prayers to the rest of the servants. Some weeks afterwards,
happening to pass late in the evening by an outhouse, he saw
and heard one of his men reading the Bible with difficulty
by the light of the fire, to the others. After this the party
knelt and prayed: in their prayers they mentioned Mr.
THE VOYAGE OF THE BEAGLE 453
Bushby and his family, and the missionaries, each separately
in his respective district
December 26th. — Mr. Bushby offered to take Mr. Sulivan
and myself in his boat some miles up the river to Cawa-
Cawa; and proposed afterwards to walk on to the village of
Waiomio, where there are some curious rocks. Following
one of the arms of the bay, we enjoyed a pleasant row, and
passed through pretty scenery, until we came to a village,
beyond which the boat could not pass. From this place a
chief and a party of men volunteered to walk with us to
Waiomio, a distance of four miles. The chief was at this
time rather notorious from having lately hung one of his
wives and a slave for adultery. When one of the mission-
aries remonstrated with him he seemed surprised, and said
he thought he was exactly following the English method.
Old Shongi, who happened to be in England during the
Queen's trial, expressed great disapprobation at the whole
proceeding: he said he had five wives, and he would rather
cut off all their heads than be so much troubled about one.
Leaving this village, we crossed over to another, seated on
a hill-side at a little distance. The daughter of a chief, who
was still a heathen, had died there five days before. The
hovel in which she had expired had been burnt to the ground :
her body being enclosed between two small canoes, was
placed upright on the ground, and protected by an enclosure
bearing wooden images of their gods, and the whole was
painted bright red, so as to be conspicuous from afar. Her
gown was fastened to the coffin, and her hair being cut off
was cast at its foot. The relatives of the family had torn
the flesh of their arms, bodies, and faces, so that they were
covered with clotted blood; and the old women looked most
filthy, disgusting objects. On the following day some of the
officers visited this place, and found the women still howling
and cutting themselves.
We continued our walk, and soon reached Waiomio. Here
there are some singular masses of limestone, resembling
ruined castles. These rocks have long served for burial
places, and in consequence are held too sacred to be ap-
proached. One of the young men, however, cried out, " Let
us all be brave/' and ran on ahead ; but when within a hun-
454 CHARLES DARWIN
dred yards, the whole party thought better of it, and stopped
short. With perfect indifference, however, they allowed us
to examine the whole place. At this village we rested some
hours, during which time there was a long discussion with
Mr. Bushby, concerning the right of sale of certain lands.
One old man, who appeared a perfect genealogist, illustrated
the successive possessors by bits of stick driven into the
ground. Before leaving the houses a little basketful of
roasted sweet potatoes was given to each of our party; and
we all, according to the custom, carried them away to eat
on the road. I noticed that among the women employed in
cooking, there was a man-slave: it must be a humiliating
thing for a man in this warlike country to be employed in
doing that which is considered as the lowest woman's work.
Slaves are not allowed to go to war; but this perhaps can
hardly be considered as a hardship. I heard of one poor
wretch who, during hostilities, ran away to the opposite
party; being met by two men, he was immediately seized;
but as they could not agree to whom he should belong, each
stood over him with a stone hatchet, and seemed determined
that the other at least should not take him away alive. The
poor man, almost dead with fright, was only saved by the
address of a chief's wife. We afterwards enjoyed a pleasant
walk back to the boat, but did not reach the ship till late in
the evening.
December 30th. — In the afternoon we stood out of the
Bay of Islands, on our course to Sydney. I believe we were
all glad to leave New Zealand. It is not a pleasant place.
Amongst the natives there is absent that charming simplicity
which is found in Tahiti ; and the greater part of the English
are the very refuse of society. Neither is the country itself
attractive. I look back but to one bright spot, and that is
Waimate, with its Christian inhabitants.
CHAPTER XIX
Australia
Sydney — Excursion to Bathurst — Aspect of the Woods — Party of
Natives — Gradual Extinction of the Aborigines — Infection gener-
ated by associated Men in health — Blue Mountains — View of the
grand gulf-like Valleys — Their origin and formation — Bathurst, gen-
eral civility of the Lower Orders — State of Society — Van Diemen's
Land — Hobart Town — Aborigines all banished — Mount Wellington
— King George's Sound — Cheerless Aspect of the Country — Bald
Head, calcareous casts of branches of Trees — Party of Natives —
Leave Australia.
y'ANUARY 12th, 1836. — Early in the morning a light air
carried us towards the entrance of Port Jackson. In-
stead of beholding a verdant country, interspersed with
fine houses, a straight line of yellowish cliff brought to our
minds the coast of Patagonia. A solitary lighthouse, built of
white stone, alone told us that we were near a great and
populous city. Having entered the harbour, it appears fine
and spacious, with cliff-formed shores of horizontally strati-
fied sandstone. The nearly level country is covered with thin
scrubby trees, bespeaking the curse of sterility. Proceeding
further inland, the country improves: beautiful villas and
nice cottages are here and there scattered along the beach.
In the distance stone houses, two and three stories high, and
windmills standing on the edge of a bank, pointed out to us
the neighbourhood of the capital of Australia.
At last we anchored within Sydney Cove. We found the
little basin occupied by many large ships, and surrounded by
warehouses. In the evening I walked through the town, and
returned full of admiration at the whole scene. It is a most
magnificent testimony to the power of the British nation.
Here, in a less promising country, scores of years have done
many more times more than an equal number of centuries
have effected in South America. My first feeling was to
congratulate myself that I was born an Englishman. Upon
455
456 CHARLES DARWIN
seeing more of the town afterwards, perhaps my admiration
fell a little ; but yet it is a fine town. The streets are regular,
broad, clean, and kept in excellent order; the houses are of a
good size, and the shops well furnished. It may be faithfully
compared to the large suburbs which stretch out from London
and a few other great towns in England; but not even near
London or Birmingham is there an appearance of such rapid
growth. The nuinber of large houses and other buildings just
finished was truly surprising; nevertheless, every one com-
plained of the high rents and difficulty in procuring a house.
Coming from South America, where in the towns every man
of property is known, no one thing surprised me more than
not being able to ascertain at once to whom this or that car-
riage belonged.
I hired a man and two horses to take me to Bathurst, a
village about one hundred and twenty miles in the interior,
and the centre of a great pastoral district. By this means I
hoped to gain a general idea of the appearance of the country.
On the morning of the 16th (January) I set out on my excur-
sion. The first stage took us to Paramatta, a small country
town, next to Sydney in importance. The roads were excel-
lent, and made upon the MacAdam principle, whinstone hav-
ing been brought for the purpose from the distance of several
miles. In all respects there was a close resemblance to Eng-
land: perhaps the alehouses here were more numerous. The
iron gangs, or parties of convicts who have committed here
some offense, appeared the least like England: they were
working in chains, under the charge of sentries with loaded
arms.
The power which the government possesses, by means
of forced labour, of at once opening good roads throughout
the country, has been, I believe, one main cause of the early
prosperity of this colony. I slept at night at a very com-
fortable inn at Emu ferry, thirty-five miles from Sydney,
and near the ascent of the Blue Mountains. This line of
road is the most frequented, and has been the longest in-
habited of any in the colony. The whole land is enclosed
with high railings, for the farmers have not succeeded in
rearing hedges. There are many substantial houses and good
cottages scattered about; but although considerable pieces of
THE VOYAGE OF THE BEAGLE 457
land are under cultivation, the greater part yet remains as
when first discovered.
The extreme uniformity of the vegetation is the most
remarkable feature in the landscape of the greater part of
New South Wales. Everywhere we have an open woodland,
the ground being partially covered with a very thin pasture,
with little appearance of verdure. The trees nearly all
belong to one family, and mostly have their leaves placed in
a vertical, instead of, as in Europe, in a nearly horizontal
position : the foliage is scanty, and of a peculiar pale green
tint; without any gloss. Hence the woods appear light and
shadowless : this, although a loss of comfort to the traveller
under the scorching rays of summer, is of importance to the
farmer, as it allows grass to grow where it otherwise would
not. The leaves are not shed periodically: this character
appears common to the entire southern hemisphere, namely,
South America, Australia, and the Cape of Good Hope. The
inhabitants of this hemisphere, and of the intertropical
regions, thus lose perhaps one of the most glorious, though
to our eyes common, spectacles in the world — the first burst-
ing into full foliage of the leafless tree.^ They may, however,
say that we pay dearly for this by having the land covered
with mere naked skeletons for so many months. This is too
true; but our senses thus acquire a keen relish for the ex-
quisite green of the spring, which the eyes of those living
within the tropics, sated during the long year with the gor-
geous productions of those glowing climates, can never ex-
perience. The greater number of the trees, with the excep-
tion of some of the Blue-gums, do not attain a large size;
but they grow tall and tolerably straight, and stand well
apart. The bark of some of the Eucalypti falls annually, or
hangs dead in long shreds which swing about with the wind,
and give to the woods a desolate and untidy appearance. I
cannot imagine a more complete contrast, in every respect,
than between the forests of Valdivia or Chiloe, and the
woods of Australia.
At sunset, a party of a score of the black aborigines passed
by, each carrying, in their accustomed manner, a bundle of
spears and other weapons. By giving a leading young man a
shilling, they were easily detained, and threw their spears for
458 CHARLES DARWIN
my amusement. They were all partly clothed, and several
could speak a little English: their countenances were good-
humoured and pleasant, and they appeared far from being
such utterly degraded beings as they have usually been repre-
sented. In their own arts they are admirable. A cap being
fixed at thirty yards distance, they transfixed it with a spear,
delivered by the throwing-stick with the rapidity of an arrow
from the bow of a practised archer. In tracking animals or
men they show most wonderful sagacity ; and I heard of sev-
eral of their remarks which manifested considerable acute-
ness. They will not, however, cultivate the ground, or build
houses and remain stationary, or even take the trouble of
tending a flock of sheep when given to them. On the whole
they appear to me to stand some few degrees higher in the
scale of civilization than the Fuegians.
It is very curious thus to see in the midst of a civilized
people, a set of harmless savages wandering about without
knowing where they shall sleep at night, and gaining their
livelihood by hunting in the woods. As the white man has
travelled onwards, he has spread over the country belonging
to several tribes. These, although thus enclosed by one com-
mon people, keep up their ancient distinctions, and some-
times go to war with each other. In an engagement which
took place lately, the two parties most singularly chose the
centre of the village of Bathurst for the field of battle. This
was of service to the defeated side, for the runaway warriors
took refuge in the barracks.
The number of aborigines is rapidly decreasing. In my
whole ride, with the exception of some boys brought up by
Englishmen, I saw only one other party. This decrease, no
doubt, must be partly owing to the introduction of spirits, to
European diseases (even the milder ones of which, such as
the measles, 1 prove very destructive), and to the gradual
extinction of the wild animals. It is said that numbers of
their children invariably perish in very early infancy from
the effects of their wandering life; and as the difficulty of
1 It is remarkable how the same disease is modified in different climates.
At the little island of St. Helena the introduction of scarlet fever is dreaded
as a plague. In some countries, foreigners and natives are as differently
affected by certain contagious disorders as if they had been different ani-
mals; of which fact some instances have occurred in Chile; and, according
to Humboldt, in Mexico (Polit. Essay, New Spain, vol. iv.).
THE VOYAGE OF THE BEAGLE 459
procuring food increases, so must their wandering habits
increase; and hence the population, without any apparent
deaths from famine, is repressed in a manner extremely
sudden compared to what happens in civilized countries,
where the father, though in adding to his labour he may in-
jure himself, does not destroy his offspring.
Besides the several evident causes of destruction, there
appears to be some more mysterious agency generally at
work. Wherever the European has trod, death seems to pur-
sue the aboriginal. We may look to the wide extent of the
Americas, Polynesia, the Cape of Good Hope, and Australia,
and we find the same result. Nor is it the white man alone
that thus acts the destroyer ; the Polynesian of Malay extrac-
tion has in parts of the East Indian archipelago, thus driven
before him the dark-coloured native. The varieties of man
seem to act on each other in the same way as different species
of animals — the stronger always extirpating the weaker. It
was melancholy at New Zealand to hear the fine energetic
natives saying, that they knew the land was doomed to pass
from their children. Every one has heard of the inexplicable
reduction of the population in the beautiful and healthy island
of Tahiti since the date of Captain Cook's voyages : although
in that case we might have expected that it would have been
increased; for infanticide, which formerly prevailed to so
extraordinary a degree, has ceased; profligacy has greatly
diminished, and the murderous wars become less frequent.
The Rev. J. Williams, in his interesting work 2 , says, that
the first intercourse between natives and Europeans, " is in-
variably attended with the introduction of fever, dysentery,
or some other disease, which carries off numbers of the peo-
ple. ,, Again he affirms, " It is certainly a fact, which cannot
be controverted, that most of the diseases which have raged
in the islands during my residence there, have been intro-
duced by ships; 3 and what renders this fact remarkable is,
3 Narrative of Missionary Enterprise, p. 282.
f Captain Beechey (chap, iv., vol. i.) states that the inhabitants of Pit-
cairn Island are firmly convinced that after the arrival of every ship they
suffer cutaneous and other disorders. Captain Beechey attributes this to
the change of diet during the time of the visit. Dr. Macculloch (Western
Isles, vol. ii. p. 32) says: " It is asserted, that on the arrival of a stranger
(at St. Kilda) all the inhabitants, in the common phraseology, catch a
cold." Dr. Macculloch considers the whole case, although often previously
affirmed, as ludicrous. He adds, however, that " the question was put by
460 CHARLES DARWIN
that there might be no appearance of disease among the crew
of the ship which conveyed this destructive importation. ,,
This statement is not quite so extraordinary as it at first
appears; for several cases are on record of the most malig-
nant fevers having broken out, although the parties them-
selves, who were the cause, were not affected. In the early
part of the reign of George III., a prisoner who had been
confined in a dungeon, was taken in a coach with four con-
stables before a magistrate; and although the man himself
was not ill, the four constables died from a short putrid
fever; but the contagion extended to no others. From these
facts it would almost appear as if the effluvium of one set
of men shut up for some time together was poisonous when
inhaled by others; and possibly more so, if the men be of
different races. Mysterious as this circumstance appears to
be, it is not more surprising than that the body of one's
fellow-creature, directly after death, and before putrefaction
has commenced, should often be of so deleterious a quality,
that the mere puncture from an instrument used in its dis-
section, should prove fatal.
17th. — Early in the morning we passed the Nepean in a
ferry-boat. The river, although at this spot both broad and
deep, had a very small body of running water. Having
crossed a low piece of land on the opposite side, we reached
the slope of the Blue Mountains. The ascent is not steep,
the road having been cut with much care on the side of a
sandstone cliff. On the summit an almost level plain extends,
which, rising imperceptibly to the westward, at last attains
a height of more than 3000 feet. From so grand a title as
Blue Mountains, and from their absolute altitude, I expected
to have seen a bold chain of mountains crossing the coun-
us to the inhabitants who unanimously agreed in the story." In Vancou-
ver's Voyage, there is a somewhat similar statement with respect to Otaheitc
Dr. Dieffenbach, in a note to his translation of this Journal, states that the
same fact is universally believed by the inhabitants of the Chatham Islands,
and in parts of New Zealand. It is impossible that such a belief should
have become universal in the northern hemisphere, at the Antipodes, and
in the Pacific, without some good foundation. Humboldt (Polit. Essay on
King of New Spain, vol. iv.) says, that the great epidemics of Panama and
Callao are " marked " by the arrival of ships from Chile, because the people
from that temperate region, first experience the fatal effects of the torrid
zones. I may add, that I have heard it stated in Shropshire, that sheep,
which have been imported from vessels, although themselves in a healthy
condition, if placed in the same fold with others, frequently produce sick-
ness in the flock.
THE VOYAGE OF THE BEAGLE 461
try; but instead of this, a sloping plain presents merely an
inconsiderable front to the low land near the coast. From
this first slope, the view of the extensive woodland to the
east was striking, and the surrounding trees grew bold and
lofty. But when once on the sandstone platform, the scenery
becomes exceedingly monotonous; each side of the road is
bordered by scrubby trees of the never-failing Eucalyptus
family; and with the exception of two or three small inns,
there are no houses or cultivated land: the road, moreover,
is solitary; the most frequent object being a bullock-waggon,
piled up with bales of wool.
In the middle of the day we baited our horses at a little
inn, called the Weatherboard. The country here is elevated
2800 feet above the sea. About a mile and a half from this
place there is a view exceedingly well worth visiting. Fol-
lowing down a little valley and its tiny rill of water, an
immense gulf unexpectedly opens through the trees which
border the pathway, at the depth of perhaps 1500 feet.
Walking on a few yards, one stands on the brink of a vast
precipice, and below one sees a grand bay or gulf, for I know
not what other name to give it, thickly covered with forest.
The point of view is situated as if at the head of a bay, the
line of cliff diverging on each side, and showing headland
behind headland, as on a bold sea-coast. These cliffs are
composed of horizontal strata of whitish sandstone; and
are so absolutely vertical, that in many places a person
standing on the edge and throwing down a stone, can see it
strike the trees in the abyss below. So unbroken is the line
of cliff, that in order to reach the foot of the waterfall,
formed by this little stream, it is said to be necessary to go
sixteen miles round. About five miles distant in front,
another line of cliff extends, which thus appears completely
to encircle the valley; and hence the name of bay is justified,
as applied to this grand amphitheatrical depression. If we
imagine a winding harbour, with its deep water surrounded
by bold cliff-like shores, to be laid dry, and a forest to spring
up on its sandy bottom, we should then have the appearance
and structure here exhibited. This kind of view was to me
quite novel, and extremely magnificent.
In the evening we reached the Blackheath. The sand-
462 CHARLES DARWIN
stone plateau has here attained the height of 3400 feet; and
is covered, as before, with the same scrubby woods. From
the road, there were occasional glimpses into a profound
valley, of the same character as the one described; but from
the steepness and depth of its sides, the bottom was scarcely
ever to be seen. The Blackheath is a very comfortable inn,
kept by an old soldier ; and it reminded me of the small inns
in North Wales.
18th. — Very early in the morning, I walked about three
miles to see Govetfs Leap; a view of a similar character
with that near the Weatherboard, but perhaps even more
stupendous. So early in the day the gulf was filled with a
thin blue haze, which, although destroying the general effect
of the view added to the apparent depth at which the forest
was stretched out beneath our feet. These valleys, which so
long presented an insuperable barrier to the attempts of the
most enterprising of the colonists to reach the interior, are
most remarkable. Great arm-like bays, expanding at their
upper ends, often branch from the main valleys and pen-
etrate the sandstone platform; on the other hand, the plat-
form often sends promontories into the valleys, and even
leaves in them great, almost insulated, masses. To descend
into some of these valleys, it is necessary to go round twenty
miles; and into others, the surveyors have only lately pen-
etrated, and the colonists have not yet been able to drive in
their cattle. But the most remarkable feature in their struc-
ture is, that although several miles wide at their heads, they
generally contract towards their mouths to such a degree
as to become impassable. The Surveyor-General, Sir T.
Mitchell, 4 endeavoured in vain, first walking and then by
crawling between the great fallen fragments of sandstone,
to ascend through the gorge by which the river Grose joins
the Nepean; yet the valley of the Grose in its upper part,
as I saw, forms a magnificent level basin some miles in
width, and is on all sides surrounded by cliffs, the summits
of which are believed to be nowhere less than 3000 feet
above the level of the sea. When cattle are driven into the
valley of the Wolgan by a path (which I descended), partly
4 Travels in Australia, vol. i. p. 154. I must express my obligation to
Sir T. Mitchell, for several interesting personal communications on the
subject of these great valleys of New South Wales.
THE VOYAGE OF THE BEAGLE 463
natural and partly made by the owner of the land, they can-
not escape ; for this valley is in every other part surrounded
by perpendicular cliffs, and eight miles lower down, it con-
tracts from an average width of half a mile, to a mere
chasm, impassable to man or beast. Sir T. Mitchell states
that the great valley of the Cox river with all its branches,
contracts, where it unites with the Nepean, into a gorge
2200 yards in width, and about iooo feet in depth. Other
similar cases might have been added.
The first impression, on seeing the correspondence of the
horizontal strata on each side of these valleys and great
amphitheatrical depressions, is that they have been hollowed
out, like other valleys, by the action of water; but when one
reflects on the enormous amount of stone, which on this
view must have been removed through mere gorges or
chasms, one is led to ask whether these spaces may not have
subsided. But considering the form of the irregularly
branching valleys, and of the narrow promontories projecting
into them from the platforms, we are compelled to abandon
this notion. To attribute these hollows to the present allu-
vial action would be preposterous; nor does the drainage
from the summit-level always fall, as I remarked near the
Weatherboard, into the head of these valleys, but into one
side of their bay-like recesses. Some of the inhabitants re-
marked to me that they never viewed one of those bay-like
recesses, with the headlands receding on both hands, without
being struck with their resemblance to a bold sea-coast. This
is certainly the case ; moreover, on the present coast of New
South Wales, the numerous, fine, widely-branching harbours,
which are generally connected with the sea by a narrow
mouth worn through the sandstone coast-cliffs, varying from
one mile in width to a quarter of a mile, present a likeness,
though on a miniature scale, to the great valleys of the
interior. But then immediately occurs the startling difficulty,
why has the sea worn out these great, though circumscribed
depressions on a wide platform, and left mere gorges at the
openings, through which the whole vast amount of triturated
matter must have been carried away? The only light I can
throw upon this enigma, is by remarking that banks of the
most irregular forms appear to be now forming in some seas,
464 CHARLES DARWIN
as in parts of the West Indies and in the Red Sea, and that
their sides are exceedingly steep. Such banks, I have been
led to suppose, have been formed by sediment heaped by
strong currents on an irregular bottom. That in some cases
the sea, instead of spreading out sediment in a uniform sheet,
heaps it round submarine rocks and islands, it is hardly pos-
sible to doubt, after examining the charts of the West Indies;
and that the waves have power to form high and precipitous
cliffs, even in land-locked harbours, I have noticed in many
parts of South America. To apply these ideas to the sand-
stone platforms of New South Wales, I imagine that the
strata were heaped by the action of strong currents, and of
the undulations of an open sea, on an irregular bottom; and
that the valley-like spaces thus left unfilled had their steeply
sloping flanks worn into cliffs, during a slow elevation of
the land; the worn-down sandstone being removed, either at
the time when the narrow gorges were cut by the retreating
sea, or subsequently by alluvial action.
Soon after leaving the Blackheath, we descended from the
sandstone platform by the pass of Mount Victoria. To effect
this pass, an enormous quantity of stone has been cut
through; the design, and its manner of execution, being
worthy of any line of road in England. We now entered
upon a country less elevated by nearly a thousand feet, and
consisting of granite. With the change of rock, the vegeta-
tion improved; the trees were both finer and stood farther
apart ; and the pasture between them was a little greener and
more plentiful. At Hassan's Walls, I left the high road,
and made a short detour to a farm called Walerawang; to
the superintendent of which I had a letter of introduction
from the owner in Sydney. Mr. Browne had the kindness to
ask me to stay the ensuing day, which I had much pleasure
in doing. This place offers an example of one of the large
farming, or rather sheep-grazing establishments of the
colony. Cattle and horses are, however, in this case rather
more numerous than usual, owing to some of the valleys
being swampy and producing a coarser pasture. Two or
three flat pieces of ground near the house were cleared and
cultivated with corn, which the harvest-men were now reap-
THE VOYAGE OF THE BEAGLE 465
ing: but no more wheat is sown than sufficient for the annual
support of the labourers employed on the establishment. The
usual number of assigned convict-servants here is about
forty, but at the present time there were rather more. Al-
though the farm was well stocked with every necessary,
there was an apparent absence of comfort; and not one
single woman resided here. The sunset of a fine day will
generally cast an air of happy contentment on any scene;
but here, at this retired farm-house, the brightest tints on
the surrounding woods could not make me forget that forty
hardened, profligate men were ceasing from their daily
labours, like the slaves from Africa, yet without their holy
claim for compassion.
Early on the next morning, Mr. Archer, the joint superin-
tendent, had the kindness to take me out kangaroo-hunting.
We continued riding the greater part of the day, but had
very bad sport, not seeing a kangaroo, or even a wild dog.
The greyhounds pursued a kangaroo rat into a hollow tree,
out of which we dragged it: it is an animal as large as a
rabbit, but with the figure of a kangaroo. A few years since
this country abounded with wild animals; but now the emu
is banished to a long distance, and the kangaroo is become
scarce; to both the English greyhound has been highly de-
structive. It may be long before these animals are altogether
exterminated, but their doom is fixed. The aborigines are
always anxious to borrow the dogs from the farm-houses:
the use of them, the offal when an animal is killed, and some
milk from the cows, are the peace-offerings of the settlers,
who push farther and farther towards the interior. The
thoughtless aboriginal, blinded by these trifling advantages,
is delighted at the approach of the white man, who seems
predestined to inherit the country of his children.
Although having poor sport, we enjoyed a pleasant ride.
The woodland is generally so open that a person on horse-
back can gallop through it. It is traversed by a few flat-
bottomed valleys, which are green and free from trees: in
such spots the scenery was pretty like that of a park. In the
whole country I scarcely saw a place without the marks of a
fire ; whether these had been more or less recent — whether
the stump6 were more or less black, was the greatest change
466 CHARLES DARWIN
which varied the uniformity, so wearisome to the traveller's
eye. In these woods there are not many birds; I saw, how-
ever, some large flocks of the white cockatoo feeding in a
corn-field, and a few most beautiful parrots; crows, like our
jackdaws were not uncommon, and another bird something
like the magpie. In the dusk of the evening I took a stroll
along a chain of ponds, which in this dry country represented
the course of a river, and had the good fortune to see several
of the famous Ornithorhynchus paradoxus. They were
diving and playing about the surface of the water, but
showed so little of their bodies, that they might easily have
been mistaken for water-rats. Mr. Browne shot one: cer-
tainly it is a most extraordinary animal ; a stuffed specimen
does not at all give a good idea of the appearance of the
head and beak when fresh; the latter becoming hard and
contracted. 5
20th. — A long day's ride to Bathurst. Before joining the
highroad we followed a mere path through the forest; and
the country, with the exception of a few squatters' huts, was
very solitary. We experienced this day the sirocco-like wind
of Australia, which comes from the parched deserts of the
interior. Clouds of dust were travelling in every direction;
and the wind felt as if it had passed over a fire. I after-
wards heard that the thermometer out of doors had stood at
119 , and in a closed room at 96 . In the afternoon we came
in view of the downs of Bathurst. These undulating but
nearly smooth plains are very remarkable in this country,
from being absolutely destitute of trees. They support only
a thin brown pasture. We rode some miles over this coun-
try, and then reached the township of Bathurst, seated in the
middle of what may be called either a very broad valley, or
narrow plain. I was told at Sydney not to form too bad an
opinion of Australia by judging of the country from the road-
side, nor too good a one from Bathurst ; in this latter respect,
5 I was interested by finding here the hollow conical pitfall of the lion-
ant, or some other insect; first a fly fell down the treacherous slope and
immediately disappeared; then came a large but unwary ant; its struggles
to escape being very violent, those curious little jets of sand, described by
Kirby and Spence (Entomol., vol. i. p. 425) as being flirted by the insect's
tail, were promptly directed against the expected victim. But the ant
enjoyed a better fate than the fly, and escaped the fatal jaws which lay
concealed at the base of the conical hollow. This Australian pitfall was
only about half the size of that made by the European lion ant.
THE VOYAGE OF THE BEAGLE 467
I did not feel myself in the least danger of being preju-
diced. The season, it must be owned, had been one of great
drought, and the country did not wear a favourable aspect;
although I understand it was incomparably worse two or
three months before. The secret of the rapidly growing
prosperity of Bathurst is, that the brown pasture which
appears to the stranger's eye so wretched, is excellent for
sheep-grazing. The town stands, at the height of 2200 feet
above the sea, on the banks of the Macquarie. This is one of
the rivers flowing into the vast and scarcely known interior.
The line of watershed, which divides the inland streams from
those on the coast, has a height of about 3000 feet, and runs
in a north and south direction at the distance of from eighty
to a hundred miles from the sea-side. The Macquarie figures
in the map as a respectable river, and it is the largest of
those draining this part of the water-shed ; yet to my surprise
I found it a mere chain of ponds, separated from each other
by spaces almost dry. Generally a small stream is running;
and sometimes there are high and impetuous floods. Scanty
as the supply of the water is throughout this district, it
becomes still scantier further inland.
22nd. — I commenced my return, and followed a new road
called Lockyer's Line, along which the country is rather more
hilly and picturesque. This was a long day's ride; and the
house where I wished to sleep was some way off the road,
and not easily found. I met on this occasion, and indeed on
all others, a very general and ready civility among the lower
orders, which, when one considers what they are, and what
they have been, would scarcely have been expected. The
farm where I passed the night, was owned by two young
men who had only lately come out, and were beginning a
settler's life. The total want of almost every comfort was
not attractive; but future and certain prosperity was before
their eyes, and that not far distant.
The next day we passed through large tracts of country in
flames, volumes of smoke sweeping across the road. Before
noon we joined our former road, and ascended Mount Vic-
toria. I slept at the Weatherboard, and before dark took
another walk to the amphitheatre. On the road to Sydney
I spent a very pleasant evening with Captain King at Dun-
468 CHARLES DARWIN
heved; and thus ended my little excursion in the colony of
New South Wales.
Before arriving here the three things which interested me
most were — the state of society amongst the higher classes,
the condition of the convicts, and the degree of attraction
sufficient to induce persons to emigrate. Of course, after
so very short a visit, one's opinion is worth scarcely any-
thing; but it is as difficult not to form some opinion, as it is
to form a correct judgment. On the whole, from what I
heard, more than from what I saw, I was disappointed in the
state of society. The whole community is rancorously
divided into parties on almost every subject. Among those
who, from their station in life, ought to be the best, many
live in such open profligacy that respectable people cannot
associate with them. There is much jealousy between the
children of the rich emancipist and the free settlers, the
former being pleased to consider honest men as interlopers.
The whole population, poor and rich, are bent on acquiring
wealth: amongst the higher orders, wool and sheep-grazing
form the constant subject of conversation. There are many
serious drawbacks to the comforts of a family, the chief of
which, perhaps, is being surrounded by convict servants.
How thoroughly odious to every feeling, to be waited on by
a man who the day before, perhaps, was flogged, from your
representation, for some trifling misdemeanor. The female
servants are of course, much worse: hence children learn the
vilest expressions, and it is fortunate, if not equally vile
ideas.
On the other hand, the capital of a person, without any
trouble on his part, produces him treble interest to what it
will in England ; and with care he is sure to grow rich. The
luxuries of life are in abundance, and very little dearer than
in England, and most articles of food are cheaper. The
climate is splendid, and perfectly healthy; but to my mind
its charms are lost by the uninviting aspect of the country.
Settlers possess a great advantage in finding their sons of
service when very young. At the age of from sixteen to
twenty, they frequently take charge of distant farming sta-
tions. This, however, must happen at the expense of their
boys associating entirely with convict servants. I am not
THE VOYAGE OF THE BEAGLE 469
aware that the tone of society has assumed any peculiar
character; but with such habits, and without intellectual
pursuits, it can hardly fail to deteriorate. My opinion is
such, that nothing but rather sharp necessity should compel
me to emigrate.
The rapid prosperity and future prospects of this colony
are to me, not understanding these subjects, very puzzling.
The two main exports are wool and whale-oil, and to both
of these productions there is a limit. The country is totally
unfit for canals, therefore there is a not very distant point,
beyond which the land-carriage of wool will not repay the
expense of shearing and tending sheep. Pasture everywhere
is so thin that settlers have already pushed far into the
interior: moreover, the country further inland becomes ex-
tremely poor. Agriculture, on account of the droughts, can
never succeed on an extended scale: therefore, so far as I
can see, Australia must ultimately depend upon being the
centre of commerce for the southern hemisphere, and per-
haps on her future manufactories. Possessing coal, she
always has the moving power at hand. From the habitable
country extending along the coast, and from her English
extraction, she is sure to be a maritime nation. I formerly
imagined that Australia would rise to be as grand and power-
ful a country as North America, but now it appears to me
that such future grandeur is rather problematical.
With respect to the state of the convicts, I had still fewer
opportunities of judging than on other points. The first
question is, whether their condition is at all one of punish-
ment: no one will maintain that it is a very severe one.
This, however, I suppose, is of little consequence as long as
it continues to be an object of dread to criminals at home.
The corporeal wants of the convicts are tolerably well sup-
plied: their prospect of future liberty and comfort is not
distant, and, after good conduct, certain. A " ticket of
leave," which, as long as a man keeps clear of suspicion as
well as of crime, makes him free within a certain district, is
given upon good conduct, after years proportional to the
length of the sentence; yet with all this, and overlooking
the previous imprisonment and wretched passage out, I
believe the years of assignment are passed away with discon-
470 CHARLES DARWIN
tent and unhappiness. As an intelligent man remarked to
me, the convicts know no pleasure beyond sensuality, and in
this they are not gratified. The enormous bribe which Gov-
ernment possesses in offering free pardons, together with the
deep horror of the secluded penal settlements, destroys con-
fidence between the convicts, and so prevents crime. As to a
sense of shame, such a feeling does not appear to be known,
and of this I witnessed some very singular proofs. Though
it is a curious fact, I was universally told that the character
of the convict population is Qne of arrant cowardice: not
unfrequently some become desperate, and quite indifferent as
to life, yet a plan requiring cool or continued courage is
seldom put into execution. The worst feature in the whole
case is, that although there exists what may be called a legal
reform, and comparatively little is committed which the law
can touch, yet that any moral reform should take place
appears to be quite out of the question. I was assured by
well-informed people, that a man who should try to improve,
could not while living with other assigned servants; — his
life would be one of intolerable misery and persecution. Nor
must the contamination of the convict-ships and prisons, both
here and in England, be forgotten. On the whole, as a place
of punishment, the object is scarcely gained; as a real system
of reform it has failed, as perhaps would every other plan;
but as a means of making men outwardly honest, — of con-
verting vagabonds, most useless in one hemisphere, into
active citizens of another, and thus giving birth to a new
and splendid country — a grand centre of civilization — it has
succeeded to a degree perhaps unparalleled in history.
30th. — The Beagle sailed for Hobart Town in Van Die-
men's Land. On the 5th of February, after a six days' pas-
sage, of which the first part was fine, and the latter very cold
and squally, we entered the mouth of Storm Bay: the weather
justified this awful name. The bay should rather be called
an estuary, for it receives at its head the waters of the Der-
went. Near the mouth, there are some extensive basaltic
platforms ; but higher up the land becomes mountainous, and
is covered by a light wood. The lower parts of the hills
which skirt the bay are cleared; and the bright yellow fields
THE VOYAGE OF THE BEAGLE 471
of corn, and dark green ones of potatoes, appear very lux-
uriant. Late in the evening we anchored in the snug cove,
on the shores of which stands the capital of Tasmania. The
first aspect of the place was very inferior to that of Sydney ;
the latter might be called a city, this is only a town. It
stands at the base of Mount Wellington, a mountain 3100
feet high, but of little picturesque beauty; from this source,
however, it receives a good supply of water. Round the cove
there are some fine warehouses, and on one side a small fort.
Coming from the Spanish settlements, where such magnifi-
cent care has generally been paid to the fortifications, the
means of defence in these colonies appeared very contempti-
ble. Comparing the town with Sydney, I was chiefly struck
with the comparative fewness of the large houses, either
built or building. Hobart Town, from the census of 1835,
contained 13,826 inhabitants, and the whole of Tasmania
36,505.
All the aborigines have been removed to an island in
Bass's Straits, so that Van Diemen's Land enjoys the great
advantage of being free from a native population. This
most cruel step seems to have been quite unavoidable, as
the only means of stopping a fearful succession of robberies,
burnings, and murders, committed by the blacks; and which
sooner or later would have ended in their utter destruction.
I fear there is no doubt, that this train of evil and its conse-
quences, originated in the infamous conduct of some of
our countrymen. Thirty years is a short period, in which to
have banished the last aboriginal from his native island, —
and that island nearly as large as Ireland. The correspond-
ence on this subject, which took place between the government
at home and that of Van Diemen's Land, is very interesting.
Although numbers of natives were shot and taken prisoners
in the skirmishing, which was going on at intervals for sev-
eral years ; nothing seems fully to have impressed them with
the idea of our overwhelming power, until the whole island,
in 1830, was put under martial law, and by proclamation the
whole population commanded to assist in one great attempt
to secure the entire race. The plan adopted was nearly simi-
lar to that of the great hunting-matches in India : a line was
formed reaching across the island, with the intention of
472 CHARLES DARWIN
driving the natives into a cul-de-sac on Tasman's peninsula.
The attempt failed; the natives, having tied up their dogs,
stole during one night through the lines. This is far from
surprising, when their practised senses, and usual manner
of crawling after wild animals is considered. I have been
assured that they can conceal themselves on almost bare
ground, in a manner which until witnessed is scarcely credi-
ble; their dusky bodies being easily mistaken for the black-
ened stumps which are scattered all over the country. I was
told of a trial between a party of Englishmen and a native,
who was to stand in full view on the side of a bare hill ; if the
Englishmen closed their eyes for less than a minute, he
would squat down, and then they were never able to distin-
guish him from the surrounding stumps. But to return to
the hunting-match; the natives understanding this kind of
warfare, were terribly alarmed, for they at once perceived
the power and numbers of the whites. Shortly afterwards
a party of thirteen belonging to two tribes came in; and,
conscious of their unprotected condition, delivered them-
selves up in despair. Subsequently by the intrepid exertions
of Mr. Robinson, an active and benevolent man, who
fearlessly visited by himself the most hostile of the natives,
the whole were induced to act in a similar manner. They
were then removed to an island, where food and clothes
were provided them. Count Strzelecki states, 6 that " at the
epoch of their deportation in 1835, the number of natives
amounted to 210. In 1842, that is, after the interval of seven
years, they mustered only fifty- four individuals; and, while
each family of the interior of New South Wales, uncontami-
nated by contact with the whites, swarms with children, those
of Flinders' Island had during eight years an accession of
only fourteen in number ! "
The Beagle stayed here ten days, and in this time I made
several pleasant little excursions, chiefly with the object of
examining the geological structure of the immediate neigh-
bourhood. The main points of interest consist, first in some
highly fossiliferous strata, belonging to the Devonian or
Carboniferous period; secondly, in proofs of a late small rise
of the land; and lastly, in a solitary and superficial patch of
• Physical Description of New South Wales and Van Diemen's Land, p.354«
THE VOYAGE OF THE BEAGLE 473
yellowish limestone or travertin, which contains numerous
impressions of leaves of trees, together with land-shells, not
now existing. It is not improbable that this one small quarry
includes the only remaining record of the vegetation of Van
Diemen's Land during one former epoch.
The climate here is damper than in New South Wales,
and hence the land is more fertile. Agriculture flourishes:
the cultivated fields look well, and the gardens abound with
thriving vegetables and fruit-trees. Some of the farm-
houses, situated in retired spots, had a very attractive ap-
pearance. The general aspect of the vegetation is similar to
that of Australia ; perhaps it is a little more green and cheer-
ful; and the pasture between the trees rather more abun-
dant. One day I took a long walk on the side of the bay op-
posite to the town : I crossed in a steamboat, two of which
are constantly plying backwards and forwards. The ma-
chinery of one of these vessels was entirely manufactured in
this colony, which, from its very foundation, then numbered
only three and thirty years ! Another day I ascended Mount
Wellington; I took with me a guide, for I failed in a first
attempt, from the thickness of the wood. Our guide, how-
ever, was a stupid fellow, and conducted us to the southern
and damp side of the mountain, where the vegetation was
very luxuriant ; and where the labour of the ascent, from the
number of rotten trunks, was almost as great as on a moun-
tain in Tierra del Fuego or in Chiloe. It cost us five and a
half hours of hard climbing before we reached the summit.
In many parts the Eucalypti grew to a great size, and com-
posed a noble forest. In some of the dampest ravines, tree-
ferns flourished in an extraordinary manner; I saw one
which must have been at least twenty feet high to the base
of the fronds, and was in girth exactly six feet. The fronds
forming the most elegant parasols, produced a gloomy shade,
like that of the first hour of the night. The summit of the
mountain is broad and flat, and is composed of huge angular
masses of naked greenstone. Its elevation is 3100 feet above
the level of the sea. The day was splendidly clear, and we
enjoyed a most extensive view ; to the north, the country ap-
peared a mass of wooded mountains, of about the same height
with that on which we were standing, and with an equally
474 CHARLES DARWIN
tame outline: to the south the broken land and water, form-
ing many intricate bays, was mapped with clearness before
us. After staying some hours on the summit, we found a
better way to descend, but did not reach the Beagle till eight
o'clock, after a severe day's work.
February jth. — The Beagle sailed from Tasmania, and,
on the 6th of the ensuing month, reached King George's
Sound, situated close to the S. W. corner of Australia. We
stayed there eight days; and we did not during our voyage
pass a more dull and uninteresting time. The country,
viewed from an eminence, appears a woody plain, with here
and there rounded and partly bare hills of granite protrud-
ing. One day I went out with a party, in hopes of seeing a
kangaroo hunt, and walked over a good many miles of coun-
try. Everywhere we found the soil sandy, and very poor;
it supported either a coarse vegetation of thin, low brush-
wood and wiry grass, or a forest of stunted trees. The
scenery resembled that of the high sandstone platform of the
Blue Mountains; the Casuarina (a tree somewhat resem-
bling a Scotch fir) is, however, here in greater number, and
the Eucalyptus in rather less. In the open parts there were
many grass-trees, — a plant which, in appearance, has some
affinity with the palm; but, instead of being surmounted by
a crown of noble fronds, it can boast merely of a tuft of
very coarse grass-like leaves. The general bright green col-
our of the brushwood and other plants, viewed from a dis-
tance, seemed to promise fertility. A single walk, however,
was enough to dispel such an illusion; and he who thinks
with me will never wish to walk again in so uninviting a
country.
One day I accompanied Captain Fitz Roy to Bald Head;
the place mentioned by so many navigators, where some im-
agined that they saw corals, and others that they saw petri-
fied trees, standing in the position in which they had grown.
According to our view, the beds have been formed by the
wind having heaped up fine sand, composed of minute round-
ed particles of shells and corals, during which process
branches and roots of trees, together with many land-shells,
became enclosed. The whole then became consolidated by
the percolation of calcareous matter; and the cylindrical
THE VOYAGE OF THE BEAGLE 475
cavities left by the decaying of the wood, were thus also
filled up with a hard pseudo-stalactical stone. The weather
is now wearing away the softer parts, and in consequence
the hard casts of the roots and branches of the trees project
above the surface, and, in a singularly deceptive manner, re-
semble the stumps of a dead thicket.
A large tribe of natives, called the White Cockatoo men,
happened to pay the settlement a visit while we were there.
These men, as well as those of the tribe belonging to King
George's Sound, being tempted by the offer of some tubs of
rice and sugar, were persuaded to hold a " corrobery," or
great dancing-party. As soon as it grew dark, small fires
were lighted, and the men commenced their toilet, which
consisted in painting themselves white in spots and lines.
As soon as all was ready, large fires were kept blazing,
round which the women and children were collected as spec-
tators ; the Cockatoo and King George's men formed two dis-
tinct parties, and generally danced in answer to each other.
The dancing consisted in their running either sideways or in
Indian file into an open space, and stamping the ground with
great force as they marched together. Their heavy foot-
steps were accompanied by a kind of grunt, by beating their
clubs and spears together, and by various other gesticula-
tions, such as extending their arms and wriggling their
bodies. It was a most rude, barbarous scene, and, to our
ideas, without any sort of meaning; but we observed that
the black women and children watched it with the greatest
pleasure. Perhaps these dances originally represented actions,
such as wars and victories; there was one called the Emu
dance, in which each man extended his arm in a bent man-
ner, like the neck of that bird. In another dance, one man
imitated the movements of a kangaroo grazing in the woods,
whilst a second crawled up, and pretended to spear him.
When both tribes mingled in the dance, the ground trembled
with the heaviness of their steps, and the air resounded with
their wild cries. Every one appeared in high spirits, and the
group of nearly naked figures, viewed by the light of the
blazing fires, all moving in hideous harmony, formed a per-
fect display of a festival amongst the lowest barbarians. In
Tierra del Fuego, we have beheld many curious scenes in
476 CHARLES DARWIN
savage life, but never, I think, one where the natives were
in such high spirits, and so perfectly at their ease. After
the dancing was over, the whole party formed a great circle
on the ground, and the boiled rice and sugar was distributed,
to the delight of all.
After several tedious delays from clouded weather, on the
14th of March, we gladly stood out of King George's Sound
on our course to Keeling Island. Farewell, Australia! you
are a rising child, and doubtless some day will reign a great
princess in the South: but you are too great and ambitious
for affection, yet not great enough for respect. I leave your
shores without sorrow or regret.
CHAPTER XX
Keeling Island: — Coral Formations
Keeling Island — Singular appearance — Scanty Flora — Transport of
Seeds — Birds and Insects — Ebbing and flowing Springs — Fields of
dead Coral — Stones transported in the roots of Trees — Great Crab
— Stinging Corals — Coral-eating Fish — Coral Formations — Lagoon
Islands, or Atolls — Depth at which reef-building Corals can live —
Vast Areas interspersed with low Coral Islands — Subsidence of
their foundations — Barrier Reefs — Fringing Reefs — Conversion of
Fringing Reefs into Barrier Reefs, and into Atolls — Evidence of
changes in Level — Breaches in Barrier Reefs — Maldiva Atolls ;
their peculiar structure — Dead and submerged Reefs — Areas of
subsidence and elevation — Distribution of Volcanoes — Subsidence
slow, and vast in amount.
APRIL ist. — We arrived in view of the Keeling or
A\ Cocos Islands, situated in the Indian Ocean, and
about six hundred miles distant from the coast of
Sumatra. This is one of the lagoon-islands (or atolls) of
coral formation, similar to those in the Low Archipelago
which we passed near. When the ship was in the channel
at the entrance, Mr. Liesk, an English resident, came off in
his boat. The history of the inhabitants of this place, in
as few words as possible, is as follows. About nine years
ago, Mr. Hare, a worthless character, brought from the East
Indian archipelago a number of Malay slaves, which now,
including children, amount to more than a hundred. Shortly
afterwards, Captain Ross, who had before visited these isl-
ands in his merchant-ship, arrived from England, bringing
with him his family and goods for settlement: along with
him came Mr. Liesk, who had been a mate in his vessel.
The Malay slaves soon ran away from the islet on which
Mr. Hare was settled, and joined Captain Ross's party. Mr.
Hare upon this was ultimately obliged to leave the place.
The Malays are now nominally in a state of freedom, and
certainly are so, as far as regards their personal treatment;
477
478 CHARLES DARWIN
but in most other points they are considered as slaves. From
their discontented state, from the repeated removals from
islet to islet, and perhaps also from a little mismanagement,
things are not very prosperous. The island has no domestic
quadruped, excepting the pig, and the main vegetable pro-
duction is the cocoa-nut. The whole prosperity of the place
depends on this tree : the only exports being oil from the nut,
and the nuts themselves, which are taken to Singapore and
Mauritius, where they are chiefly used, when grated, in mak-
ing curries. On the cocoa-nut, also, the pigs, which are
loaded with fat, almost entirely subsist, as do the ducks and
poultry. Even a huge land-crab is furnished by nature with
the means to open and feed on this most useful production.
The ring-formed reef of the lagoon-island is surmounted
in the greater part of its length by linear islets. On the
northern or leeward side, there is an opening through which
vessels can pass to the anchorage within. On entering, the
scene was very curious and rather pretty; its beauty, how-
ever, entirely depended on the brilliancy of the surrounding
colours. The shallow, clear, and still water of the lagoon,
resting in its greater part on white sand, is, when illumined
by a vertical sun, of the most vivid green. This brilliant
expanse, several miles in width, is on all sides divided, either
by a line of snow-white breakers from the dark heaving
waters of the ocean, or from the blue vault of heaven by
the strips of land, crowned by the level tops of the cocoa-
nut trees. As a white cloud here and there affords a pleas-
ing contrast with the azure sky, so in the lagoon, bands of
living coral darken the emerald green water.
The next morning after anchoring, I went on shore on
Direction Island. The strip of dry land is only a few hun-
dred yards in width ; on the lagoon side there is a white cal-
careous beach, the radiation from which under this sultry
climate was very oppressive ; and on the outer coast, a solid
broad flat of coral-rock served to break the violence of the
open sea. Excepting near the lagoon, where there is some
sand, the land is entirely composed of rounded fragments of
coral. In such a loose, dry, stony soil, the climate of the
intertropical regions alone could produce a vigorous vegeta-
tion. On some of the smaller islets, nothing could be more
THE VOYAGE OF THE BEAGLE 479
elegant than the manner in which the young and full-grown
cocoa-nut trees, without destroying each other's symmetry,
were mingled into one wood. A beach of glittering white
sand formed a border to these fairy spots.
I will now give a sketch of the natural history of these
islands, which, from its very paucity, possesses a peculiar
interest. The cocoa-nut tree, at the first glance, seems to
compose the whole wood; there are, however, five or six
other trees. One of these grows to a very large size, but
from the extreme softness of its wood, is useless; another
sort affords excellent timber for ship-building. Besides the
trees, the number of plants is exceedingly limited, and con-
sists of insignificant weeds. In my collection, which in-
cludes, I believe, nearly the perfect Flora, there are twenty
species, without reckoning a moss, lichen, and fungus. To
this number two trees must be added ; one of which was not
in flower, and the other I only heard of. The latter is a
solitary tree of its kind, and grows near the beach, where,
without doubt, the one seed was thrown up by the waves. A
Guilandina also grows on only one of the islets. I do not
include in the above list the sugar-cane, banana, some other
vegetables, fruit-trees, and imported grasses. As the islands
consist entirely of coral, and at one time must have existed
as mere water-washed reefs, all their terrestrial productions
must have been transported here by the waves of the sea.
In accordance with this, the Florula has quite the character
of a refuge for the destitute: Professor Henslow informs
me that of the twenty species nineteen belong to different
genera, and these again to no less than sixteen families I 1
In Holman's 2 Travels an account is given, on the author-
ity of Mr. A. S. Keating, who resided twelve months on these
islands, of the various seeds and other bodies which have
been known to have been washed on shore. " Seeds and
plants from Sumatra and Java have been driven up by the
surf on the windward side of the islands. Among them have
been found the Kimiri, native of Sumatra and the peninsula
of Malacca; the cocoa-nut of Balci, known by its shape and
size; the Dadass, which is planted by the Malays with the
1 These plants are described in the Annals of Nat. Hist, vol. i., 1838,
P. 337-
2 Holman's Travels, vol. iv. p. 378.
480 CHARLES DARWIN
pepper-vine, the latter intwining round its trunk, and sup-
porting itself by the prickles on its stem; the soap-tree; the
castor-oil plant ; trunks of the sago palm ; and various kinds
of seeds unknown to the Malays settled on the islands.
These are all supposed to have been driven by the N. W.
monsoon to the coast of New Holland, and thence to these
islands by the S. E. trade-wind. Large masses of Java teak
and Yellow wood have also been found, besides immense
trees of red and white cedar, and the blue gumwood of New
Holland, in a perfectly sound condition. All the hardy seeds,
such as creepers, retain their germinating power, but the
softer kinds, among which is the mangostin, are destroyed
in the passage. Fishing-canoes, apparently from Java, have
at times been washed on shore." It is interesting thus to
discover how numerous the seeds are, which, coming from
several countries, are drifted over the wide ocean. Pro-
fessor Henslow tells me, he believes that nearly all the plants
which I brought from these islands, . are common littoral
species in the East Indian archipelago. From the direction,
however, of the winds and currents, it seems scarcely pos-
sible that they could have come here in a direct line. If,
as suggested with much probability by Mr. Keating, they
were first carried towards the coast of New Holland, and
thence drifted back together with the productions of that
country, the seeds, before germinating, must have travelled
between 1800 and 2400 miles.
Chamisso, 8 when describing the Radack Archipelago, situ-
ated in the western part of the Pacific, states that " the sea
brings to these islands the seeds and fruits of many trees,
most of which have yet not grown here. The greater part
of these seeds appear to have not yet lost the capability of
growing.''
It is also said that palms and bamboos from some-
where in the torrid zone, and trunks of northern firs, are
washed on shore: these firs must have come from an im-
mense distance. These facts are highly interesting. It can-
not be doubted that if there were land-birds to pick up the
seeds when first cast on shore, and a soil better adapted for
their growth than the loose blocks of coral, that the most
8 Kotzebue's First Voyage, vol. iii. p. 155.
THE VOYAGE OF THE BEAGLE 481
isolated of the lagoon-islands would in time possess a far
more abundant Flora than they now have.
The list of land animals is even poorer than that of the
plants. Some of the islets are inhabited by rats, which were
brought in a ship from the Mauritius, wrecked here. These
rats are considered by Mr. Waterhouse as identical with the
English kind, but they are smaller, and more brightly col-
oured. There are no true land-birds ; for a snipe and a rail
(Rallus Phillippensis), though living entirely in the dry
herbage, belong to the order of Waders. Birds of this order
are said to occur on several of the small low islands in the
Pacific. At Ascension, where there is no land-bird, a rail
(Porphyrio simplex) was shot near the summit of the moun-
tain, and it was evidently a solitary straggler. At Tristan
d'Acunha, where, according to Carmichael, there are only
two land-birds, there is a coot. From these facts I believe
that the waders, after the innumerable web-footed species,
are generally the first colonists of small isolated islands. I
may add, that whenever I noticed birds, not of oceanic
species, very far out at sea, they always belonged to this
order; and hence they would naturally become the earliest
colonists of any remote point of land.
Of reptiles I saw only one small lizard. Of insects I took
pains to collect every kind. Exclusive of spiders, which were
numerous, there were thirteen species.* Of these, one only
was a beetle. A small ant swarmed by thousands under the
loose dry blocks of coral, and was the only true insect which
was abundant. Although the productions of the land are
thus scanty, if we look to the waters of the surrounding sea,
the number of organic beings is indeed infinite. Chamisso
has described 5 the natural history of a lagoon-island in the
Radack Archipelago; and it is remarkable how closely its
inhabitants, in number and kind, resemble those of Keeling
Island. There is one lizard and two waders, namely, a snipe
and curlew. Of plants there are nineteen species, including
a fern ; and some of these are the same with those growing
4 The thirteen species belong to the following orders: — In the Coleop-
tera, a minute Elater; Orthoptera, a Gryllus and a Blatta; Hemiptera, one
g>ecies; Homoptera, two; Neuroptera, a Chrysopa; Hymenoptera, two ants;
epidoptera nocturna, a Diopaea, and a Pterophorus (?) ; Diptera, two species.
6 Kotzebue's First Voyage, vol. iii. p. 222.
VOL. XXIX — P HC
482 CHARLES DARWIN
here, though on a spot so immensely remote, and in a dif-
ferent ocean.
The long strips of land, forming the linear islets, have
been raised only to that height to which the surf can throw
fragments of coral, and the wind heap up calcareous sand.
The solid flat of coral rock on the outside, by its breadth,
breaks the first violence of the waves, which otherwise, in a
day, would sweep away these islets and all their productions.
The ocean and the land seem here struggling for mastery:
although terra firma has obtained a footing, the denizens of
the water think their claim at least equally good. In every
part one meets hermit crabs of more than one species,® car-
rying on their backs the shells which they have stolen from
the neighbouring beach. Overhead, numerous gannets, frig-
ate-birds, and terns, rest on the trees; and the wood, from
the many nests and from the smell of the atmosphere, might
be called a sea-rookery. The gannets, sitting on their rude
nests, gaze at one with a stupid yet angry air. The noddies,
as their name expresses, are silly little creatures. But there
is one charming bird: it is a small, snow-white tern, which
smoothly hovers at the distance of a few feet above one's
head, its large black eye scanning, with quiet curiosity, your
expression. Little imagination is required to fancy that so
light and delicate a body must be tenanted by some wander-
ing fairy spirit.
Sunday, April 3rd. — After service I accompanied Captain
Fitz Roy to the settlement, situated at the distance of some
miles, on the point of an islet thickly covered with tall cocoa-
nut trees. Captain Ross and Mr. Liesk live in a large barn-
like house open at both ends, and lined with mats made of
woven bark. The houses of the Malays are arranged along
the shore of the lagoon. The whole place had rather a deso-
late aspect, for there were no gardens to show the signs of
care and cultivation. The natives belong to different islands
in the East Indian archipelago, but all speak the same lan-
guage: we saw the inhabitants of Borneo, Celebes, Java, and
8 The large claws or pincers of some of these crabs are most beautifully
adapted, when drawn back, to form an operculum to the shell, nearly as
perfect as the proper one originally belonging to the molluscous animal. I
was assured, and as far as my observation went I found it so, that certain
species of the hermit-crab always use certain species of shells.
THE VOYAGE OF THE BEAGLE 483
Sumatra. In colour they resemble the Tahitians, from whom
they do not widely differ in features. Some of the women,
however, show a good deal of the Chinese character. I liked
both their general expressions and the sound of their voices.
They appeared poor, and their houses were destitute of fur-
niture; but it was evident, from the plumpness of the little
children, that cocoa-nuts and turtle afford no bad sustenance.
On this island the wells are situated, from which ships
obtain water. At first sight it appears not a little remarkable
that the fresh water should regularly ebb and flow with the
tides ; and it has even been imagined, that sand has the power
of filtering the salt from the sea-water. These ebbing wells
are common on some of the low islands in the West Indies.
The compressed sand, or porous coral rock, is permeated like
a sponge with the salt water ; but the rain which falls on the
surface must sink to the level of the surrounding sea, and
must accumulate there, displacing an equal bulk of the salt
water. As the water in the lower part of the great sponge-
like coral mass rises and falls with the tides, so will the
water near the surface; and this will keep fresh, if the mass
be sufficiently compact to prevent much mechanical admix-
ture; but where the land consists of great loose blocks of
coral with open interstices, if a well be dug, the water, as I
have seen, is brackish.
After dinner we stayed to see a curious half superstitious
scene acted by the Malay women. A large wooden spoon
dressed in garments, and which had been carried to the grave
of a dead man, they pretend becomes inspired at the full of
the moon, and will dance and jump about. After the proper
preparations, the spoon, held by two women, became con-
vulsed, and danced in good time to the song of the surround-
ing children and women. It was a most foolish spectacle;
but Mr. Liesk maintained that many of the Malays believed
in its spiritual movements. The dance did not commence till
the moon had risen, and it was well worth remaining to be-
hold her bright orb so quietly shining through the long arms
of the cocoa-nut trees as they waved in the evening breeze.
These scenes of the tropics are in themselves so delicious,
that they almost equal those dearer ones at home, to which
we are bound by each best feeling of the mind.
484 CHARLES DARWIN
The next day I employed myself in examining the very in-
teresting, yet simple structure and origin of these islands.
The water being unusually smooth, I waded over the outer
flat of dead rock as far as the living mounds of coral, on
which the swell of the open sea breaks. In some of the
gullies and hollows there were beautiful green and other col-
oured fishes, and the form and tints of many of the zoophytes
were admirable. It is excusable to grow enthusiastic over
the infinite numbers of organic beings with which the sea of
the tropics, so prodigal of life, teems; yet I must confess I
think those naturalists who have described, in well-known
words, the submarine grottoes decked with a thousand beau-
ties, have indulged in rather exuberant language.
April 6th.— I accompanied Captain Fitz Roy to an island
at the head of the lagoon : the channel was exceedingly intri-
cate, winding through fields of delicately branched corals.
We saw several turtle and two boats were then employed in
catching them. The water was so clear and shallow, that al-
though at first a turtle quickly dives out of sight, yet in a
canoe or boat under sail, the pursuers after no very long
chase come up to it. A man standing ready in the bow, at
this moment dashes through the water upon the turtle's back ;
then clinging with both hands by the shell of its neck, he is
carried away till the animal becomes exhausted and is se-
cured. It was quite an interesting chase to see the two boats
thus doubling about, and the men dashing head foremost
into the water trying to seize their prey. Captain Moresby
informs me that in the Chagos archipelago in this same
ocean, the natives, by a horrible process, take the shell from
the back of the living turtle. " It is covered with burning
charcoal, which causes the outer shell to curl upwards; it is
then forced off with a knife, and before it becomes cold
flattened between boards. After this barbarous process the
animal is suffered to regain its native element, where, after
a certain time, a new shell is formed; it is, however, too
thin to be of any service, and the animal always appears
languishing and sickly."
When we arrived at the head of the lagoon, we crossed a
narrow islet, and found a great surf breaking on the wind-
ward coast. I can hardly explain the reason, but there is to
THE VOYAGE OF THE BEAGLE 485
my mind much grandeur in the view of the outer shores of
these lagoon-islands. There is a simplicity in the barrier-
like beach, the margin of green bushes and tall cocoa-nuts,
the solid flat of dead coral-rock, strewed here and there
with great loose fragments, and the line of furious break-
ers, all rounding away towards either hand. The ocean
throwing its waters over the broad reef appears an invinci-
ble, all-powerful enemy; yet we see it resisted, and even
conquered, by means which at first seem most weak and in-
efficient. It is not that the ocean spares the rock of coral;
the great fragments scattered over the reef, and heaped on
the beach, whence the tall cocoa-nut springs, plainly be-
speak the unrelenting power of the waves. Nor are any
periods of repose granted. The long swell caused by the
gentle but steady action of the trade-wind, always blow-
ing in one direction over a wide area, causes breakers, almost
equalling in force those during a gale of wind in the tem-
perate regions, and which never cease to rage. It is impos-
sible to behold these waves without feeling a conviction that
an island, though built of the hardest rock, let it be porphyry,
granite, or quartz, would ultimately yield and be demolished
by such an irresistible power. Yet these low, insignificant
coral-islets stand and are victorious : for here another power,
as an antagonist, takes part in the contest. The organic forces
separate the atoms of carbonate of lime, one by one, from
the foaming breakers, and unite them into a symmetrical
structure. Let the hurricane tear up its thousand huge frag-
ments ; yet what will that tell against the accumulated labour
of myriads of architects at work night and day, month after
month? Thus do we see the soft and gelatinous body of a
polypus, through the agency of the vital laws, conquering
the great mechanical power of the waves of an ocean which
neither the art of man nor the inanimate works of nature
could successfully resist.
We did not return on board till late in the evening, for we
stayed a long time in the lagoon, examining the fields of
coral and the gigantic shells of the chama, into which, if a
man were to put his hand, he would not, as long as the ani-
mal lived, be able to withdraw it. Near the head of the
lagoon I was much surprised to find a wide area, consider-
486 CHARLES DARWIN
ably more than a mile square, covered with a forest of deli-
cately branching corals, which, though standing upright,
were all dead and rotten. At first I was quite at a loss to
understand the cause; afterwards it occurred to me that it
was owing to the following rather curious combination of
circumstances. It should, however, first be stated, that corals
are not able to survive even a short exposure in the air to
the sun's rays, so that their upward limit of growth is de-
termined by that of lowest water at spring tides. It appears,
from some old charts, that the long island to windward was
formerly separated by wide channels into several islets; this
fact is likewise indicated by the trees being younger on these
portions. Under the former condition of the reef, a strong
breeze, by throwing more water over the barrier, would tend
to raise the level of the lagoon. Now it acts in a directly
contrary manner; for the water within the lagoon not only
is not increased by currents from the outside, but is itself
blown outwards by the force of the wind. Hence it is ob-
served, that the tide near the head of the lagoon does not
rise so high during a strong breeze as it does when it is
calm. This difference of level, although no doubt very small,
has, I believe, caused the death of those coral-groves, which
under the former and more open condition of the outer reef
Jhas attained the utmost possible limit of upward growth.
A few miles north of Keeling there is another small atoll,
the lagoon of which is nearly filled up with coral-mud. Cap-
tain Ross found embedded in the conglomerate on the outer
coast, a well-rounded fragment of greenstone, rather larger
than a man's head : he and the men with him were so much
surprised at this, that they brought it away and preserved it
as a curiosity. The occurrence of this one stone, where
every other particle of matter is calcareous, certainly is very
puzzling. The island has scarcely ever been visited, nor is it
probable that a ship had been wrecked there. From the ab-
sence of any better explanation, I came to the conclusion that
it must have come entangled in the roots of some large tree:
when, however, I considered the great distance from the
nearest land, the combination of chances against a stone thus
being entangled, the tree washed into the sea, floated so far,
then landed safely, and the stone finally so embedded as to
THE VOYAGE OF THE BEAGLE 487
allow of its discovery, I was almost afraid of imagining a
means of transport apparently so improbable. It was there-
fore with great interest that I found Chamisso, the justly
distinguished naturalist who accompanied Kotzebue, stating
that the inhabitants of the Radack archipelago, a group of
lagoon-islands in the midst of the Pacific, obtained stones
for sharpening their instruments by searching the roots of
trees which are cast upon the beach. It will be evident that
this must have happened several times, since laws have been
established that such stones belong to the chief, and a pun-
ishment is inflicted on any one who attempts to steal them.
When the isolated position of these small islands in the
midst of a vast ocean — their great distance from any land
excepting that of coral formation, attested by the value
which the inhabitants, who are such bold navigators, attach
to a stone of any kind, 7 — and the slowness of the currents of
the open sea, are all considered, the occurrence of pebbles
thus transported does appear wonderful. Stones may often
be thus carried ; and if the island on which they are stranded
is constructed of any other substance besides coral, they
would scarcely .attract attention, and their origin at least
would never be guessed. Moreover, this agency may long
escape discovery from the probability of trees, especially
those loaded with stones, floating beneath the surface. In
the channels of Tierra del Fuego large quantities of drift
timber are cast upon the beach, yet it is extremely rare to
meet a tree swimming on the water. These facts may pos-
sibly throw light on single stones, whether angular or
rounded, occasionally found embedded in fine sedimentary
masses.
During another day I visited West Islet, on which the
vegetation was perhaps more luxuriant than on any other.
The cocoa-nut trees generally grow separate, but here the
young ones flourished beneath their tall parents, and formed
with their long and curved fronds the most shady arbours.
Those alone who have tried it, know how delicious it is to
be seated in such shade, and drink the cool pleasant fluid
of the cocoa-nut. In this island there is a large bay-like
7 Some natives carried by Kotzebue to Kamtschatka collected stones to
take back to their country.
488 CHARLES DARWIN
space, composed of the finest white sand: it is quite level
and is only covered by the tide at high water; from this
large bay smaller creeks penetrate the surrounding woods.
To see a field of glittering white sand, representing water,
with the cocoa-nut trees extending their tall and waving
trunks around the margin, formed a singular and very pretty
view.
I have before alluded to a crab which lives on the cocoa-
nuts; it is very common on all parts of the dry land, and
grows to a monstrous size: it is closely allied or identical
with the Birgos latro. The front pair of legs terminate in
very strong and heavy pincers, and the last pair are fitted
with others weaker and much narrower. It would at first
be thought quite impossible for a crab to open a strong
cocoa-nut covered with the husk; but Mr. Liesk assures me
that he has repeatedly seen this effected. The crab begins
by tearing the husk, fibre by fibre, and always from that
end under which the three eye-holes are situated; when this
is completed, the crab commences hammering with its heavy
claws on one of the eye-holes till an opening is made. Then
turning round its body, by the aid of its posterior and nar-
row pair of pincers, it extracts the white albuminous sub-
stance. I think this is as curious a case of instinct as ever
I heard of, and likewise of adaptation in structure between
two objects apparently so remote from each other in the
scheme of nature, as a crab and a cocoa-nut tree. The
Birgos is diurnal in its habits; but every night it is said to
pay a visit to the sea, no doubt for the purpose of moistening
its branchiae. The young are likewise hatched, and live for
some time, on the coast. These crabs inhabit deep burrows,
which they hollow out beneath the roots of trees; and where
they accumulate surprising quantities of the picked fibres
of the cocoa-nut husk, on which they rest as on a bed. The
Malays sometimes take advantage of this, and collect the
fibrous mass to use as junk. These crabs are very good to
eat ; moreover, under the tail of the larger ones there is a
mass of fat, which, when melted, sometimes yields as much
as a quart bottle full of limpid oil. It has been stated by
some authors that the Birgos crawls up the cocoa-nut trees
for the purpose of stealing the nuts : I very much doubt the
THE VOYAGE OF THE BEAGLE 489
possibility of this ; but with the Pandanus 8 the task would be
very much easier. I was told by Mr. Liesk that on these
islands the Birgos lives only on the nuts which have fallen
to the ground.
Captain Moresby informs me that this crab inhabits the
Chagos and Seychelle groups, but not the neighbouring Mal-
diva archipelago. It formerly abounded at Mauritius, but
only a few small ones are now found there. In the Pacific,
this species, or one with closely allied habits, is said 9 to in-
habit a single coral island, north of the Society group. To
show the wonderful strength of the front pair of pincers, I
may mention, that Captain Moresby confined one in a strong
tin-box. which had held biscuits, the lid being secured with
wire; but the crab turned down the edges and escaped. In
turning down the edges, it actually punched many small
holes quite through the tin !
I was a good deal surprised by finding two species of
coral of the genus Millepora (M. complanata and alcicornis),
possessed of the power of stinging. The stony branches or
plates, when taken fresh from the water, have a harsh feel
and are not slimy, although possessing a strong and dis-
agreeable smell. The stinging property seems to vary in
different specimens : when a piece was pressed or rubbed on
the tender skin of the face or arm, a pricking sensation was
usually caused, which came on after the interval of a second,
and lasted only for a few minutes. One day, however, by
merely touching my face with one of the branches, pain was
instantaneously caused; it increased as usual after a few
seconds, and remaining sharp for some minutes, was percep-
tible for half an hour afterwards. The sensation was as
bad as that from a nettle, but more like that caused by the
Physalia or Portuguese man-of-war. Little red spots were
produced on the tender skin of the arm, which appeared as if
they would have formed watery pustules, but did not. M.
Quoy mentions this case of the Millepora ; and I have heard
of stinging corals in the West Indies. Many marine ani-
mals seem to have this power of stinging: besides the Portu-
guese man-of-war, many jelly-fish, and the Aplysia or sea-
8 See Proceedings of Zoological Society, 1832, p. 17.
•Tyerman and Bennett. Voyage, etc., vol. ii. p. 33.
490 CHARLES DARWIN
slug of the Cape de Verd Islands, it is stated in the voyage
of the Astrolabe, that an Actinia or sea-anemone, as well as
a flexible coralline allied to Sertularia, both possess this
means of offence or defence. In the East Indian sea, a
stinging sea-weed is said to be found.
Two species of fish, of the genus Scarus, which are com-
mon here, exclusively feed on coral: both are coloured of a
splendid bluish-green, one living invariably in the lagoon,
and the other amongst the outer breakers. Mr. Liesk assured
us, that he had repeatedly seen whole shoals grazing with
their strong bony jaws on the tops of the coral branches: I
opened the intestines of several, and found them distended
with yellowish calcareous sandy mud. The slimy disgusting
Holuthurise (allied to our star-fish), which the Chinese gour-
mands are so fond of, also feed largely, as I am informed by
Dr. Allan, on corals; and the bony apparatus within their
bodies seems well adapted for this end. These Holuthurias,
the fish, the numerous burrowing shells, and nereidous
worms, which perforate every block of dead coral, must be
very efficient agents in producing the fine white mud which
lies at the bottom and on the shores of the lagoon. A por-
tion, however, of this mud, which when wet resembled
pounded chalk, was found by Professor Ehrenberg to be
partly composed of siliceous-shielded infusoria.
April 12th. — In the morning we stood out of the lagoon
on our passage to the Isle of France. I am glad we have
visited these islands: such formations surely rank high
amongst the wonderful objects of this world. Captain Fitz
Roy found no bottom with a line 7200 feet in length, at the
distance of only 2200 yards from the shore ; hence this island
forms a lofty submarine mountain, with sides steeper even
than those of the most abrupt volcanic cone. The saucer-
shaped summit is nearly ten miles across; and every single
atom, 10 from the least particle to the largest fragment of
rock, in this great pile, which however is small compared
with very many other lagoon-islands, bears the stamp of
having been subjected to organic arrangement. We feel sur-
10 I exclude, of course, some soil which has been imported here in ves-
sels from Malacca and Java, and likewise some small fragments of pumice,
drifted here by the waves. The one block of greenstone, moreover, on the
northern island must be excepted.
THE VOYAGE OF THE BEAGLE 491
prise when travellers tell us of the vast dimensions of the
Pyramids and other great ruins, but how utterly insignificant
are the greatest of these, when compared to these moun-
tains of stone accumulated by the agency of various minute
and tender animals ! This is a wonder which does not at
first strike the eye of the body, but, after reflection, the eye
of reason.
I will now give a very brief account of the three great
classes of coral-reefs ; namely, Atolls, Barrier, and Fringing-
reefs, and will explain my views 11 on their formation. Al-
most every voyager who has crossed the Pacific has ex-
pressed his unbounded astonishment at the lagoon-islands, or
as I shall for the future call them by their Indian name of
atolls, and has attempted some explanation. Even as long
ago as the year 1605, Pyrard de Laval well exclaimed, " C'est
une merveille de voir chacun de ces atollons, environne d'un
grand banc de pierre tout autour, n'y ayant point d'artifice
humain." The accompanying sketch of Whitsunday Island
in the Pacific, copied from Capt. Beechey's admirable Voy-
age* gives but a faint idea of the singular aspect of an atoll:
it is one of the smallest size, and has its narrow islets united
together in a ring. The immensity of the ocean, the fury of
the breakers, contrasted with the lowness of the land and the
smoothness of the bright green water within the lagoon, can
hardly be imagined without having been seen.
The earlier voyagers fancied that the coral-building ani-
n These were first read before the Geological Society in May, 1837, and
have since been developed in a separate volume on the " Structure and
Distribution of Coral Reefs."
492 CHARLES DARWIN
mals instinctively built up their great circles to afford them-
selves protection in the inner parts; but so far is this from
the truth, that those massive kinds, to whose growth on the
exposed outer shores the very existence of the reef depends,
cannot live within the lagoon, where other delicately-branch-
ing kinds flourish. Moreover, on this view, many species
of distinct genera and families are supposed to combine for
one end; and of such a combination, not a single instance
can be found in the whole of nature. The theory that has
been most generally received is, that atolls are based on sub-
marine craters; but when we consider the form and size of
some, the number, proximity, and relative positions of others,
this idea loses its plausible character : thus Suadiva atoll is 44
geographical miles in diameter in one line, by 34 miles in an-
other line; Rimsky is 54 by 20 miles across, and it has a
strangely sinuous margin ; Bow atoll is 30 miles long, and on
an average only 6 in width ; Menchicoff atoll consists of three
atolls united or tied together. This theory, moreover, is to-
tally inapplicable to the northern Maldiva atolls in the Indian
Ocean (one of which is 88 miles in length, and between 10
and 20 in breadth), for they are not bounded like ordinary
atolls by narrow reefs, but by a vast number of separate
little atolls; other little atolls rising out of the great central
lagoon-like spaces. A third and better theory was advanced
by Chamisso, who thought that from the corals growing more
vigorously where exposed to the open sea, as undoubtedly is
the case, the outer edges would grow up from the general
foundation before any other part, and that this would ac-
count for the ring or cup-shaped structure. But we shall
immediately see, that in this, as well as in the crater-theory,
a most important consideration has been overlooked, namely,
on what have the reef-building corals, which cannot live at
a great depth, based their massive structures?
Numerous soundings were carefully taken by Captain Fitz
Roy on the steep outside of Keeling atoll, and it was found
that within ten fathoms, the prepared tallow at the bottom
of the lead, invariably came up marked with the impression
of living corals, but as perfectly clean as if it had been
dropped on a carpet of turf ; as the depth increased, the im-
pressions became less numerous, but the adhering particles
THE VOYAGE OF THE BEAGLE 493
of sand more and more numerous, until at last it was evident
that the bottom consisted of a smooth sandy layer : to carry
on the analogy of the turf, the blades of grass grew thinner
and thinner, till at last the soil was so sterile, that nothing
sprang from it. From these observations, confirmed by many
others, it may be safely inferred that the utmost depth at
which corals can construct reefs is between 20 and 30 fath-
oms. Now there are enormous areas in the Pacific and Indian
Ocean, in which every single island is of coral formation,
and is raised only to that height to which the waves can
throw up fragments, and the winds pile up sand. Thus
Radack group of atolls is an irregular square, 520 miles long
and 240 broad; the Low Archipelago is elliptic-formed, 840
miles in its longer, and 420 in its shorter axis: there are
other small groups and single low islands between these two
archipelagoes, making a linear space of ocean actually more
than 4000 miles in length, in which not one single island
rises above the specified height. Again, in the Indian Ocean
there is a space of ocean 1500 miles in length, including
three archipelagoes, in which every island is low and of
coral formation. From the fact of the reef-building corals
not living at great depths, it is absolutely certain that
throughout these vast areas, wherever there is now an atoll,
a foundation must have originally existed within a depth of
from 20 to 30 fathoms from the surface. It is improbable in
the highest degree that broad, lofty, isolated, steep-sided
banks of sediment, arranged in groups and lines hundreds of
leagues in length, could have been deposited in the central
and profoundest parts of the Pacific and Indian Oceans, at
an immense distance from any continent, and where the
water is perfectly limpid. It is equally improbable that the
elevatory forces should have uplifted throughout the above
vast areas, innumerable great rocky banks within 20 to 30
fathoms, or 120 to 180 feet, of the surface of the sea, and
not one single point above that level ; for where on the whole
surface of the globe can we find a single chain of mountains,
even a few hundred miles in length, with their many sum-
mits rising within a few feet of a given level, and not one
pinnacle above it? If then the foundations, whence the atoll-
building corals sprang, were not formed of sediment, and if
494 CHARLES DARWIN
they were not lifted up to the required level, they must of
necessity have subsided into it; and this at once solves the
difficulty. For as mountain after mountain, and island after
island, slowly sank beneath the water, fresh bases would be
successively afforded for the growth of the corals. It is
impossible here to enter into all the necessary details, but I
venture to defy 12 any one to explain in any other manner
how it is possible that numerous islands should be distributed
throughout vast areas — all the islands being low — all being
built of corals, absolutely requiring a foundation within a
limited depth from the surface.
Before explaining how atoll-formed reefs acquire their
peculiar structure, we must turn to the second great class,
namely, Barrier-reefs. These either extend in straight lines
in front of the shores of a continent or of a large island, or
they encircle smaller islands; in both cases, being separated
from the land by a broad and rather deep channel of water,
analogous to the lagoon within an atoll. It is remarkable
how little attention has been paid to encircling barrier-reefs ;
yet they are truly wonderful structures. The following sketch
represents part of the barrier encircling the island of Bola-
bola in the Pacific, as seen from one of the central peaks.
In this instance the whole line of reef has been converted
into land; but usually a snow-white line of great breakers,
with only here and there a single low islet crowned with
cocoa-nut trees, divides the dark heaving waters of the ocean
from the light-green expanse of the lagoon-channel. And
the quiet waters of this channel generally bathe a fringe of
low alluvial soil, loaded with the most beautiful productions
of the tropics, and lying at the foot of the wild, abrupt, cen-
tral mountains.
Encircling barrier-reefs are of all sizes, from three miles
to no less than forty-four miles in diameter; and that which
fronts one side, and encircles both ends, of New Caledonia,
is 400 miles long. Each reef includes one, two, or several
rocky islands of various heights; and in one instance, even
12 It is remarkable that Mr. Lyell, even in the first edition of his "Prin-
ciples of Geology," inferred that the amount of subsidence in the Pacific
must have exceeded that of elevation, from the area of land being very
small relatively to the agents there tending to form it, namely, the growth
of coral and volcanic action.
THE VOYAGE OF THE BEAGLE
495
as many as twelve separate islands. The reef runs at a
greater or less distance from the included land; in the
Society archipelago generally from one to three or four
miles; but at Hogoleu the reef is 20 miles on the southern
side, and 14 miles on the opposite or northern side, from the
included islands. The depth within the lagoon-channel also
varies much; from 10 to 30 fathoms may be taken as an
average; but at Vanikoro there are spaces no less than 56
fathoms or 363 feet deep. Internally the reef either slopes
gently into the lagoon-channel, or ends in a perpendicular
wall sometimes between two and three hundred feet under
water in height: externally the reef rises, like an atoll, with
extreme abruptness out of the profound depths of the ocean.
What can be more singular than these structures? We see
an island, which may be compared to a castle situated on the
summit of a lofty submarine mountain, protected by a great
wall of coral-rock, always steep externally and sometimes
internally, with a broad level summit, here and there breached
by a narrow gateway, through which the largest ships can
enter the wide and deep encircling moat.
As far as the actual reef of coral is concerned, there is not
the smallest difference, in general size, outline, grouping,
and even in quite trifling details of structure, between a
barrier and an atoll. The geographer Balbi has well remarked,
that an encircled island is an atoll with high land rising out
of its lagoon; remove the land from within, and a perfect
atoll is left.
But what has caused these reefs to spring up at such
496
CHARLES DARWIN
great distances from the shores of the included islands? It
cannot be that the corals will not grow close to the land;
for the shores within the lagoon-channel, when not sur-
rounded by alluvial soil, are often fringed by living reefs;
and we shall presently see that there is a whole class, which
I have called Fringing Reefs from their close attachment
to the shores both of continents and of islands. Again, on
what have the reef-building corals, which cannot live at
great depths, based their encircling structures? This is a
great apparent difficulty, analogous to that in the case of
atolls, which has generally been overlooked. It will be per-
ceived more clearly by inspecting the following sections,
which are real ones, taken in north and south lines, through
the islands with their barrier-reefs, of Vanikoro, Gambier,
and Maurua; and they are laid down, both vertically and
horizontally, on the same scale of a quarter of an inch to
a mile.
It should be observed that the sections might have been
taken in any direction through these islands, or through
3032 ft.
i. Vanikoro. 2. Gambier Islands. 3. Maurua.
The horizontal shading shows the barrier-reefs and lagoon-channels.
The inclined shading above the level of the sea (AA) shows the actual
form of the land; the inclined shading below this line, shows its probable
prolongation under water.
many other encircled islands, and the general features would
have been the same. Now, bearing in mind that reef-build-
ing coral cannot live at a greater depth than from 20 to 30
fathoms, and that the scale is so small that the plummets on
the right hand show a depth of 200 fathoms, on what are
THE VOYAGE OF THE BEAGLE 497
these barrier-reefs based? Are we to suppose that each
island is surrounded by a collar-like submarine ledge of rock,
or by a great bank of sediment, ending abruptly where the
reef ends?
If the sea had formerly eaten deeply into the isl-
ands, before they were protected by the reefs, thus having
left a shallow ledge round them under water, the present
shores would have been invariably bounded by great preci-
pices; but this is most rarely the case. Moreover, on this
notion, it is not possible to explain why the corals should
have sprung up, like a wall, from the extreme outer margin
of the ledge, often leaving a broad space of water within,
too deep for the growth of corals. The accumulation of a
wide, bank of sediment all round these islands, and generally
widest where the included islands are smallest, is highly im-
probable, considering their exposed positions in the central
and deepest parts of the ocean. In the case of the barrier-
reef of New Caledonia, which extends for 150 miles beyond
the northern point of the islands, in the same straight line
with which it fronts the west coast, it is hardly possible to
believe that a bank of sediment could thus have been
straightly deposited in front of a lofty island, and so far
beyond its termination in the open sea. Finally, if we look
to other oceanic islands of about the same height and of
similar geological constitution, but not encircled by coral-
reefs, we may in vain search for so trifling a circumambient
depth as 30 fathoms, except quite near to their shores; for
usually land that rises abruptly out of water, as do most of
the encircled and non-encircled oceanic islands, plunges ab-
ruptly under it. On what then, I repeat, are these barrier-
reefs based? Why, with their wide and deep moat-like chan-
nels, do they stand so far from the included land ? We shall
soon see how easily these difficulties disappear.
We come now to our third class of Fringing-reefs, which
will require a very short notice. Where the land slopes ab-
ruptly under water, these reefs are only a few yards in width,
forming a mere ribbon or fringe round the shores: where
the land slopes gently under the water the reef extends
further, sometimes even as much as a mile from the land;
but in such cases the soundings outside the reef always show
496 CHARLES DARWIN
that the submarine prolongation of the land is gently inclined.
In fact, the reefs extend only to that distance from the shore,
at which a foundation within the requisite depth from 20 to
30 fathoms is found. As far as the actual reef is concerned,
there is no essential difference between it and that forming
a barrier or an atoll : it is, however, generally of less width,
and consequently few islets have been formed on it. From
the corals growing more vigorously on the outside, and from
the noxious effect of the sediment washed inwards, the outer
edge of the reef is the highest part, and between it and the
land there is generally a shallow sandy channel a few feet in
depth. Where banks or sediments have accumulated near to
the surface, as in parts of the West Indies, they sometimes
become fringed with corals, and hence in some degree resem-
ble lagoon-islands or atolls, in the same manner as fringing-
reefs, surrounding gently sloping islands, in some degree
resemble barrier-reefs.
No theory on the formation of coral-reefs can be con-
sidered satisfactory which does not include the three great
AA. Outer edges of the fringing-reef, at the level of the sea. BB. The
shores of the fringed island.
A' A'. Outer edges of the reef, after its upward growth during a period
of subsidence, now converted into a barrier, with islets on it. B'B'. The
shores of the now encircled island. CC. Lagoon-channel.
N. B. — In this and the following woodcut, the subsidence of the land
could be represented only by an apparent rise in the level of the sea.
classes. We have seen that we are driven to believe in the
subsidence of those vast areas, interspersed with low islands,
of which not one rises above the height to which the wind and
waves can throw up matter, and yet are constructed by ani-
mals requiring a foundation, and that foundation to lie at
no great depth. Let us then take an island surrounded by
f ringing-reefs, which offer no difficulty in their structure;
THE VOYAGE OF THE BEAGLE 499
and let this island with its reefs, represented by the unbroken
lines in the woodcut, slowly subside. Now, as the island
sinks down, either a few feet at a time or quite insensibly,
we may safely infer, from what is known of the conditions
favourable to the growth of coral, that the living masses,
bathed by the surf on the margin of the reef, will soon regain
the surface. The water, however, will encroach little by little
on the shore, the island becoming lower and smaller, and the
space between the inner edge of the reef and the beach pro-
portionately broader. A section of the reef and island in this
state, after a subsidence of several hundred feet, is given by
the dotted lines. Coral islets are supposed to have been
formed on the reef; and a ship is anchored in the lagoon-
channel. This channel will be more or less deep, according
to the rate of subsidence, to the amount of sediment accumu-
lated in it, and to the growth of the delicately branched corals
which can live there. The section in this state resembles in
every respect one drawn through an encircled island : in fact,
it is a real section (on the scale of .517 of an inch to a mile)
through Bolabola in the Pacific. We can now at once see
why encircling barrier-reefs stand so far from the shores
which they front. We can also perceive, that a line drawn
perpendicularly down from the outer edge of the new reef,
to the foundation of solid rock beneath the old fringing-reef,
will exceed by as many feet as there have been feet of
subsidence, that small limit of depth at which the effective
corals can live : — the little architects having built up their
great wall-like mass, as the whole sank down, upon a basis
formed of other corals and their consolidated fragments.
Thus the difficulty on this head, which appeared so great,
disappears.
If, instead of an island, we had taken the shore of a con-
tinent fringed with reefs, and had imagined it to have sub-
sided, a great straight barrier, like that of Australia or New
Caledonia, separated from the land by a wide and deep chan-
nel, would evidently have been the result.
Let us take our new encircling barrier-reef, of which the
section is now represented by unbroken lines, and which, as
I have said, is a real section through Bolabola, and let it go
on subsiding. As the barrier-reef slowly sinks down, the
500 CHARLES DARWIN
corals will go on vigorously growing upwards; but as the
island sinks, the water will gain inch by inch on the shore —
the separate mountains first forming separate islands within
A' A'. Outer edges of the barrier-reef at the level of the sea, with islets
on it. B'B'. The shores of the included island. CC. The lagoon-channel.
A" A". Outer edges of the reef, now converted into an atoll. C. The
lagoon of the new atoll.
N. B. — According to the true scale, the depths of the lagoon-channel and
lagoon are much exaggerated.
one great reef — and finally, the last and highest pinnacle
disappearing. The instant this takes place, a perfect atoll
is formed : I have said, remove the high land from within an
encircling barrier-reef, and an atoll is left, and the land has
been removed. We can now perceive how it comes that
atolls, having sprung from encircling barrier-reefs, resemble
them in general size, form, in the manner in which they are
grouped together, and in their arrangement in single or
double lines; for they may be called rude outline charts of
the sunken islands over which they stand. We can further
see how it arises that the atolls in the Pacific and Indian
Oceans extend in lines parallel to the generally prevailing
strike of the high islands and great coast-lines of those
oceans. I venture, therefore, to affirm, that on the theory of
the upward growth of the corals during the sinking of the
land, 13 all the leading features in those wonderful structures,
the lagoon-islands or atolls, which have so long excited the
13 It has been highly satisfactory to me to find the following passage in
a pamplet by Mr. Couthouy, one of the naturalists in the great Antarctic
Expedition of the United States: — " Having personally examined a large
number of coral-islands and resided eight months among the volcanic class
having shore and partially encircling reefs. I may be permitted to state
that my own observations have impressed a conviction of the correctness
of the theory of Mr. Darwin." — The naturalists, however, of this expedi-
tion differ with me on some points respecting coral formations.
THE VOYAGE OF THE BEAGLE 501
attention of voyagers, as well as in the no less wonderful
barrier-reefs, whether encircling small islands or stretching
for hundreds of miles along the shores of a continent, are
simply explained.
It may be asked, whether I can offer any direct evidence
of the subsidence of barrier-reefs or atolls; but it must be
borne in mind how difficult it must ever be to detect a move-
ment, the tendency of which is to hide under water the part
affected. Nevertheless, at Keeling atoll I observed on all
sides of the lagoon old cocoa-nut trees undermined and fall-
ing; and in one place the foundation-posts of a shed, which
the inhabitants asserted had stood seven years before just
above high-water mark, but now was daily washed by every
tide: on inquiry I found that three earthquakes, one of them
severe, had been felt here during the last ten years. At
Vanikoro, the lagoon-channel is remarkably deep, scarcely
any alluvial soil has accumulated at the foot of the lofty
included mountains, and remarkably few islets have been
formed by the heaping of fragments and sand on the wall-
like barrier reef; these facts, and some analogous ones, led
me to believe that this island must lately have subsided and
the reef grown upwards: here again earthquakes are fre-
quent and very severe. In the Society archipelago, on the
other hand, where the lagoon-channels are almost choked up,
where much low alluvial land has accumulated, and where in
some cases long islets have been formed on the barrier-reefs
— facts all showing that the islands have not very lately
subsided — only feeble shocks are most rarely felt. In these
coral formations, where the land and water seem struggling
for mastery, it must be ever difficult to decide between the
effects of a change in the set of the tides and of a slight
subsidence: that many of these reefs and atolls are subject to
changes of some kind is certain; on some atolls the islets
appear to have increased greatly within a late period; on
others they have been partially or wholly washed away. The
inhabitants of parts of the Maldiva archipelago know the
date of the first formation of some islets; in other parts, the
corals are now flourishing on water-washed reefs, where
holes made for graves attest the former existence of inhab-
ited land. It is difficult to believe in frequent changes in the
502 CHARLES DARWIN
tidal currents of an open ocean; whereas, we have in the
earthquakes recorded by the natives on some atolls, and in
the great fissures observed on other atolls, plain evidence of
changes and disturbances in progress in the subterranean
regions.
It is evident, on our theory, that coasts merely fringed by
reefs cannot have subsided to any perceptible amount; and
therefore they must, since the growth of their corals, either
have remained stationary or have been upheaved. Now, it
is remarkable how generally it can be shown, by the presence
of upraised organic remains, that the fringed islands have
been elevated : and so far, this is indirect evidence in favour
of our theory. I was particularly struck with this fact, when
I found, to my surprise, that the descriptions given by MM.
Quoy and Gaimard were applicable, not to reefs in general
as implied by them, but only to those of the fringing class;
my surprise, however, ceased when I afterwards found that,
by a strange chance, all the several islands visited by these
eminent naturalists, could be shown by their own statements
to have been elevated within a recent geological era.
Not only the grand features in the structure of barrier-
reefs and of atolls, and to their likeness to each other in form,
size, and other characters, are explained on the theory of
subsidence — which theory we are independently forced to
admit in the very areas in question, from the necessity of
finding bases for the corals within the requisite depth — but
many details in structure and exceptional cases can thus also
be simply explained. I will give only a few instances. In
barrier-reefs it has long been remarked with surprise, that
the passages through the reef exactly face valleys in the
included land, even in cases where the reef is separated
from the land by a lagoon-channel so wide and so much
deeper than the actual passage itself, that it seems hardly
possible that the very small quantity of water or sediment
brought down could injure the corals on the reef. Now,
every reef of the fringing class is breached by a narrow
gateway in front of the smallest rivulet, even if dry during
the greater part of the year, for the mud, sand, or gravel,
occasionally washed down kills the corals on which it is
deposited. Consequently, when an island thus fringed sub-
THE VOYAGE OF THE BEAGLE 503
sides, though most of the narrow gateways will probably
become closed by the outward and upward growth of the
corals, yet any that are not closed (and some must always be
kept open by the sediment and impure water flowing out of
the lagoon-channel) will still continue to front exactly the
upper parts of those valleys, at the mouths of which the
original basal fringing-reef was breached.
We can easily see how an island fronted only on one side,
or on one side with one end or both ends encircled by barrier-
reefs, might after long-continued subsidence be converted
either into a single wall-like reef, or into an atoll with a
great straight spur projecting from it, or into two or three
atolls tied together by straight reefs — all of which excep-
tional cases actually occur. As the reef -building corals
require food, are preyed upon by other animals, are killed by
sediment, cannot adhere to a loose bottom, and may be easily
carried down to a depth whence they cannot spring up again,
we need feel no surprise at the reefs both of atolls and bar-
riers becoming in parts imperfect. The great barrier of
New Caledonia is thus imperfect and broken in many parts;
hence, after long subsidence, this great reef would not pro-
duce one great atoll 400 miles in length, but a chain or
archipelago of atolls, of very nearly the same dimension with
those in the Maldiva archipelago. Moreover, in an atoll once
breached on opposite sides, from the likelihood of the oceanic
and tidal currents passing straight through the breaches, it
is extremely improbable that the corals, especially during
continued subsidence, would ever be able again to unite the
rim; if they did not, as the whole sank downwards, one atoll
would be divided into two or more. In the Maldiva archi-
pelago there are distinct atolls so related to each other in
position, and separated by channels either unfathomable or
very deep (the channel between Ross and Ari atolls is 150
fathoms, and that between the north and south Nillandoo
atolls is 200 fathoms in depth), that it is impossible to look
at a map of them without believing that they were once
more intimately related. And in this same archipelago,
Mahlos-Mahdoo atoll is divided by a bifurcating channel
from 100 to 132 fathoms in depth, in such a manner, that
it is scarcely possible to say whether it ought strictly to
504 CHARLES DARWIN
be called three separate atolls, or one great atoll not yet
finally divided.
I will not enter on many more details ; but I must remark
that the curious structure of the northern Maldiva atolls
receives (taking into consideration the free entrance of the
sea through their broken margins) a simple explanation in
the upward and outward growth of the corals, originally
based both on small detached reefs in their lagoons, such as
occur in common atolls, and on broken portions of the linear
marginal reef, such as bounds every atoll of the ordinary
form. I cannot refrain from once again remarking on the
singularity of these complex structures — a great sandy and
generally concave disk rises abruptly from the unfathomable
ocean, with its central expanse studded, and its edge sym-
metrically bordered with oval basins of coral-rock just
lipping the surface of the sea, sometimes clothed with vege-
tation, and each containing a lake of clear water !
One more point in detail : as in the two neighbouring archi-
pelagoes corals flourish in one and not in the other, and as
so many conditions before enumerated must affect their exist-
ence, it would be an inexplicable fact if, during the changes
to which earth, air, and water are subjected, the reef -building
corals were to keep alive for perpetuity on any one spot or
area. And as by our theory the areas including atolls and
barrier-reefs are subsiding, we ought occasionally to find
reefs both dead and submerged. In all reefs, owing to the
sediment being washed out of the lagoon-channel to leeward,
that side is least favourable to the long-continued vigorous
growth of the corals; hence dead portions of reef not unfre-
quently occur on the leeward side; and these, though still
retaining their proper wall-like form, are now in several
instances sunk several fathoms beneath the surface. The
Chagos group appears from some cause, possibly from the
subsidence having been too rapid, at present to be much less
favourably circumstanced for the growth of reefs than for-
merly: one atoll has a portion of its marginal reef, nine miles
in length, dead and submerged; a second has only a few
quite small living points which rise to the surface; a third
and fourth are entirely dead and submerged; a fifth is a
mere wreck, with its structure almost obliterated. It is
THE VOYAGE OF THE BEAGLE 505
remarkable that in all these cases, the dead reefs and portions
of reef lie at nearly the same depth, namely, from six to
eight fathoms beneath the surface, as if they had been car-
ried down by one uniform movement. One of these " half-
drowned atolls/' so called by Capt. Moresby (to whom I
am indebted for much invaluable information), is of vast
size, namely, ninety nautical miles across in one direction,
and seventy miles in another line; and is in many respects
eminently curious. As by our theory it follows that new
atolls will generally be formed in each new area of sub-
sidence, two weighty objections might have been raised,
namely, that atolls must be increasing indefinitely in number ;
and secondly, that in old areas of subsidence each separate
atoll must be increasing indefinitely in thickness, if proofs
of their occasional destruction could not have been adduced.
Thus have we traced the history of these great rings of
coral-rock, from their first origin through their normal
changes, and through the occasional accidents of their exist-
ence, to their death and final obliteration.
In my volume on " Coral Formations " I have published a
map, in which I have coloured all the atolls dark-blue, the
barrier-reefs pale-blue, and the fringing reefs red. These
latter reefs have been formed whilst the land has been sta-
tionary, or, as appears from the frequent presence of upraised
organic remains, whilst it has been slowly rising: atolls and
barrier-reefs, on the other hand, have grown up during the
directly opposite movement of subsidence, which movement
must have been very gradual, and in the case of atolls so vast
in amount as to have buried every mountain-summit over
wide ocean-spaces. Now in this map we see that the reefs
tinted pale and dark-blue, which have been produced by the
same order of movement, as a general rule manifestly stand
near each other. Again we see, that the areas with the two
blue tints are of wide extent ; and that they lie separate from
extensive lines of coast coloured red, both of which circum-
stances might naturally have been inferred, on the theory of
the nature of the reefs having been governed by the nature
of the earth's movement. It deserves notice, that in more
than one instance where single red and blue circles approach
506 CHARLES DARWIN
near each other, I can show that there have been oscillations
of level ; for in such cases the red or fringed circles consist
of atolls, originally by our theory formed during subsidence,
but subsequently upheaved; and on the other hand, some of
the pale-blue or encircled islands are composed of coral-rock,
which must have been uplifted to its present height before
that subsidence took place, during which the existing barrier-
reefs grew upwards.
Authors have noticed with surprise, that although atolls
are the commonest coral-structures throughout some enor-
mous oceanic tracts, they are entirely absent in other seas,
as in the West Indies: we can now at once perceive the
cause, for where there has not been subsidence, atolls cannot
have been formed; and in the case of the West Indies and
parts of the East Indies, these tracts are known to have been
rising within the recent period. The larger areas, coloured
red and blue, are all elongated; and between the two colours
there is a degree of rude alternation, as if the rising of one
had balanced the sinking of the other. Taking into consid-
eration the proofs of recent elevation both on the fringed
coasts and on some others (for instance, in South America)
where there are no reefs, we are led to conclude that the
great continents are for the most part rising areas : and from
the nature of the coral-reefs, that the central parts of the
great oceans are sinking areas. The East Indian archipelago,
the most broken land in the world, is in most parts an area
of elevation, but surrounded and penetrated, probably in
more lines than one, by narrow areas of subsidence.
I have marked with vermilion spots all the many known
active volcanos within the limits of this same map. Their
entire absence from every one of the great subsiding areas,
coloured either pale or dark blue, is most striking and not
less so is the coincidence of the chief volcanic chains with
the parts coloured red, which we are led to conclude have
either long remained stationary, or more generally have been
recently upraised. Although a few of the vermilion spots
occur within no great distance of single circles tinted blue,
yet not one single active volcano is situated within several
hundred miles of an archipelago, or even small group of
atolls. It is, therefore, a striking fact that in the Friendly
THE VOYAGE OF THE BEAGLE 507
archipelago, which consists of a group of atolls upheaved
and since partially worn down, two volcanos, and perhaps
more, are historically known to have been in action. On the
other hand, although most of the islands in the Pacific which
are encircled by barrier-reefs, are of volcanic origin, often
with the remnants of craters still distinguishable, not one of
them is known to have ever been in eruption. Hence in these
cases it would appear, that volcanos burst forth into action
and become extinguished on the same spots, accordingly as
elevatory or subsiding movements prevail there. Numberless
facts could be adduced to prove that upraised organic remains
are common wherever there are active volcanos ; but until it
could be shown that in areas of subsidence, volcanos were
either absent or inactive, the inference, however probable in
itself, that their distribution depended on the rising or falling
of the earth's surface, would have been hazardous. But now,
I think, we may freely admit this important deduction.
Taking a final view of the map, and bearing in mind the
statements made with respect to the upraised organic remains,
we must feel astonished at the vastness of the areas, which
have suffered changes in level either downwards or upwards,
within a period not geologically remote. It would appear
also, that the elevatory and subsiding movements follow
nearly the same laws. Throughout the spaces interspersed
with atolls, where not a single peak of high land has been
left above the level of the sea, the sinking must have been
immense in amount. The sinking, moreover, whether con-
tinuous, or recurrent with intervals sufficiently long for the
corals again to bring up their living edifices to the surface,
must necessarily have been extremely slow. This conclusion
is probably the most important one which can be deduced
from the study of coral formations ; — and it is one which it is
difficult to imagine how otherwise could ever have been ar-
rived at. Nor can I quite pass over the probability of the
former existence of large archipelagoes of lofty islands,
where now only rings of coral-rock scarcely break the open
expanse of the sea, throwing some light on the distribution of
the inhabitants of the other high islands, now left standing
so immensely remote from each other in the midst of the
great oceans. The reef-constructing corals have indeed
508 CHARLES DARWIN
reared and preserved wonderful memorials of the subter-
ranean oscillations of level; we see in each barrier-reef a
proof that the land has there subsided, and in each atoll a
monument over an island now lost. We may thus, like unto
a geologist who had lived his ten thousand years and kept a
record of the passing changes, gain some insight into the
great system by which the surface of this globe has been
broken up, and land and water interchanged.
CHAPTER XXI
Mauritius to England
Mauritius, beautiful appearance of — Great crateriform ring of Moun-
tains — Hindoos — St. Helena — History of the changes in the Vege-
tation — Cause of the extinction of Land-shells — Ascension — Vari-
ation in the imported Rats — Volcanic Bombs — Beds of Infusoria —
Bahia — Brazil — Splendour of Tropical Scenery — Pernambuco —
Singular Reef — Slavery — Return to England — Retrospect on our
Voyage.
A PRIL 29th. — In the morning we passed round the
/-\ northern end of Mauritius, or the Isle of France.
From this point of view the aspect of the island
equalled the expectations raised by the many well-known
descriptions of its beautiful scenery. The sloping plain of
the Pamplemousses, interspersed with houses, and coloured
by the large fields of sugar-cane of a bright green, composed
the foreground. The brilliancy of the green was the more
remarkable because it is a colour which generally is con-
spicuous only from a very short distance. Towards the cen-
tre of the island groups of wooded mountains rose out of
this highly cultivated plain ; their summits, as so commonly
happens with ancient volcanic rocks, being jagged into the
sharpest points. Masses of white clouds were collected
around these pinnacles, as if for the sake of pleasing the
stranger's eye. The whole island, with its sloping border
and central mountains, was adorned with an air of perfect
elegance: the scenery, if I may use such an expression, ap-
peared to the sight harmonious.
I spent the greater part of the next day in walking about
the town and visiting different people. The town is of con-
siderable size, and is said to contain 20,000 inhabitants ; the
streets are very clean and regular. Although the island has
been so many years under the English Government, the gen-
eral character of the place is quite French: Englishmen
509
510 CHARLES DARWIN
speak to their servants in French, and the shops are all
French; indeed, I should think that Calais or Boulogne was
much more Anglified. There is a very pretty little theatre,
in which operas are excellently performed. We were also
surprised at seeing large booksellers' shops, with well-stored
shelves; — music and reading bespeak our approach to the
old world of civilization; for in truth both Australia and
America are new worlds.
The various races of men walking in the streets afford the
most interesting spectacle in Port Louis. Convicts from
India are banished here for life; at present there are about
800, and they are employed in various public works. Before
seeing these people, I had no idea that the inhabitants of
India were such noble-looking figures. Their skin is ex-
tremely dark, and many of the older men had large mus-
taches and beards of a snow-white colour ; this, together with
the fire of their expression, gave them quite an imposing
aspect. The greater number had been banished for murder
and the worst crimes; others for causes which can scarcely
be considered as moral faults, such as for not obeying, from
superstitious motives, the English laws. These men are
generally quiet and well-conducted; from their outward
conduct, their cleanliness, and faithful observance of their
strange religious rites, it was impossible to look at them
with the same eyes as on our wretched convicts in New
South Wales.
May 1st. — Sunday. I took a quiet walk along the sea-
coast to the north of the town. The plain in this part is quite
uncultivated; it consists of a field of black lava, smoothed
over with coarse grass and bushes, the latter being chiefly
Mimosas. The scenery may be described as intermediate in
character between that of the Galapagos and of Tahiti; but
this will convey a definite idea to very few persons. It is a
very pleasant country, but it has not the charms of Tahiti, or
the grandeur of Brazil. The next day I ascended La Pouce,
a mountain so called from a thumb-like projection, which
rises close behind the town to a height of 2,600 feet. The
centre of the island consists of a great platform, surrounded
by old broken basaltic mountains, with their strata dipping
seawards. The central platform, formed of comparatively
THE VOYAGE OF THE BEAGLE 511
recent streams of lava, is of an oval shape, thirteen geo-
graphical miles across, in the line of its shorter axis. The
exterior bounding mountains come into that class of struc-
tures called Craters of Elevation, which are supposed to have
been formed not like ordinary craters, but by a great and
sudden upheaval. There appears to me to be insuperable
objections to this view: on the other hand, I can hardly
believe, in this and in some other cases, that these marginal
crateriform mountains are merely the basal remnants of
immense volcanos, of which the summits either have been
blown off, or swallowed up in subterranean abysses.
From our elevated position we enjoyed an excellent view
over the island. The country on this side appears pretty well
cultivated, being divided into fields and studded with farm-
houses. I was, however, assured that of the whole land, not
more than half is yet in a productive state; if such be the
case, considering the present large export of sugar, this
island, at some future period when thickly peopled, will be
of great value. Since England has taken possession of it, a
period of only twenty-five years, the export of sugar is said
to have increased seventy-five fold. One great cause of its
prosperity is the excellent state of the roads. In the neigh-
bouring Isle of Bourbon, which remains under the French
government, the roads are still in the same miserable state
as they were here only a few years ago. Although the
French residents must have largely profited by the increased
prosperity of their island, yet the English government is far
from popular.
3rd. — In the evening Captain Lloyd, the Surveyor-general,
so well known from his examination of the Isthmus of Pana-
ma, invited Mr. Stokes and myself to his country-house,
which is situated on the edge of Wilheim Plains, and about
six miles from the Port. We stayed at this delightful place
two days ; standing nearly 800 feet above the sea, the air was
cool and fresh, and on every side there were delightful walks.
Close by, a grand ravine has been worn to a depth of about
500 feet through the slightly inclined streams of lava, which
have flowed from the central platform.
5^ —Captain Lloyd took us to the Riviere Noire, which is
several miles to the southward, that I might examine some
512 CHARLES DARWIN
rocks of elevated coral. We passed through pleasant gar-
dens, and fine fields of sugar-cane growing amidst huge
blocks of lava. The roads were bordered by hedges of
Mimosa, and near many of the houses there were avenues
of the mango. Some of the views, where the peaked hills
and the cultivated farms were seen together, were exceed-
ingly picturesque; and we were constantly tempted to
exclaim, " How pleasant it would be to pass one's life in
such quiet abodes ! " Captain Lloyd possessed an elephant,
and he sent it half way with us, that we might enjoy a ride
in true Indian fashion. The circumstance which sur-
prised me most was its quite noiseless step. This elephant
is the only one at present on the island ; but it is said others
will be sent for.
May pth. — We sailed from Port Louis, and, calling at the
Cape of Good Hope, on the 8th of July, we arrived off St.
Helena. This island, the forbidding aspect of which has
been so often described, rises abruptly like a huge black
castle from the ocean. Near the town, as if to complete
nature's defence, small forts and guns fill up every gap in
the rugged rocks. The town runs up a flat and narrow
valley; the houses look respectable, and are interspersed
with a very few green trees. When approaching the anchor-
age there was one striking view : an irregular castle perched
on the summit of a lofty hill, and surrounded by a few scat-
tered fir-trees, boldly projected against the sky.
The next day I obtained lodgings within a stone's throw
of Napoleon's tomb; 1 it was a capital central situation,
whence I could make excursions in every direction. During
the four days I stayed here, I wandered over the island from
morning to night, and examined its geological history. My
lodgings were situated at a height of about 2000 feet; here
the weather was cold and boisterous, with constant showers
of rain ; and every now and then the whole scene was veiled
in thick clouds.
1 After the volumes of eloquence which have poured forth on this sub-
ject, it is dangerous even to mention the tomb. A modern traveller, in
twelve lines, burdens the poor little island with the following titles, — it
is a grave, tomb, pyramid, cemetery, sepulchre, catacomb, sarcophagus,
minaret, and mausoleum!
THE VOYAGE OF THE BEAGLE 513
Near the coast the rough lava is quite bare : in the central
and higher parts, feldspathic rocks by their decomposition
have produced a clayey soil, which, where not covered by
vegetation, is stained in broad bands of many bright colours.
At this season, the land moistened by constant showers, pro-
duces a singularly bright green pasture, which lower and
lower down, gradually fades away and at last disappears.
In latitude i6°, and at the trifling elevation of 1500 feet, it is
surprising to behold a vegetation possessing a character
decidedly British. The hills are crowned with irregular
plantations of Scotch firs; and the sloping banks are thickly
scattered over with thickets of gorse, covered with its bright
yellow flowers. Weeping-willows are common on the banks
of the rivulets, and the hedges are made of the blackberry,
producing its well-known fruit. When we consider that the
number of plants now found on the island is 746, and that
out of these fifty-two alone are indigenous species, the rest
having been imported, and most of them from England,
we see the reason of the British character of the vegetation.
Many of these English plants appear to flourish better than
in their native country ; some also from the opposite quarter
of Australia succeed remarkably well. The many imported
species must have destroyed some of the native kinds; and
it is only on the highest and steepest ridges that the indig-
enous Flora is now predominant.
The English, or rather Welsh character of the scenery, is
kept up by the numerous cottages and small white houses;
some buried at the bottom of the deepest valleys, and others
mounted on the crests of the lofty hills. Some of the views
are striking, for instance that from near Sir W. Doveton's
house, where the bold peak called Lot is seen over a dark
wood of firs, the whole being backed by the red water-worn
mountains of the southern coast. On viewing the island
from an eminence, the first circumstance which strikes one,
is the number of the roads and forts: the labour bestowed
on the public works, if one forgets its character as a prison,
seems out of all proportion to its extent or value. There
is so little level or useful land, that it seems surprising how
so many people, about 5000, can subsist here. The lower
orders, or the emancipated slaves, are I believe extremely
vol. xxix — Q hc
514 CHARLES DARWIN
poor: they complain of the want of work. From the reduc-
tion in the number of public servants, owing to the island
having been given up by the East Indian Company, and the
consequent emigration of many of the richer people, the
poverty probably will increase. The chief food of the work-
ing class is rice with a little salt meat; as neither of these
articles are the products of the island, but must be purchased
with money, the low wages tell heavily on the poor people.
Now that the people are blessed with freedom, a right which
I believe they value fully, it seems probable that their num-
bers will quickly increase: if so, what is to become of the
little state of St. Helena?
My guide was an elderly man, who had been a goatherd
when a boy, and knew every step amongst the rocks. He
was of a race many times crossed, and although with a
dusky skin, he had not the disagreeable expression of a
mulatto. He was a very civil, quiet old man, and such
appears the character of the greater number of the lower
classes. It was strange to my ears to hear a man, nearly
white and respectably dressed, talking with indifference of
the times when he was a slave. With my companion, who
carried our dinners and a horn of water, which is quite
necessary, as all the water in the lower valleys is saline, I
every day took long walks.
Beneath the upper and central green circle, the wild val-
leys are quite desolate and untenanted. Here, to the geolo-
gist, there were scenes of high interest, showing successive
changes and complicated disturbances. According to my
views, St. Helena has existed as an island from a very
remote epoch: some obscure proofs, however, of the eleva-
tion of the land are still extant. I believe that the central
and highest peaks form parts of the rim of a great crater,
the southern half of which has been entirely removed by the
waves of the sea: there is, moreover, an external wall of
black basaltic rocks, like the coast-mountains of Mauritius,
which are older than the central volcanic streams. On the
higher parts of the island, considerable numbers of a shell,
long thought to be a marine species, occur imbedded in the
soil.
It proved to be a Cochlogena, or land-shell of a very
THE VOYAGE OF THE BEAGLE 515
peculiar form; 2 with it I found six other kinds; and in
another spot an eighth species. It is remarkable that none
of them are now found living. Their extinction has prob-
ably been caused by the entire destruction of the woods, and
the consequent loss of food and shelter, which occurred
during the early part of the last century.
The history of the changes, which the elevated plains of
Longwood and Deadwood have undergone, as given in Gen-
eral Beatson's account of the island, is extremely curious.
Both plains, it is said in former times were covered with
wood, and were therefore called the Great Wood. So late
as the year 1716 there were many trees, but in 1724 the old
trees had mostly fallen; and as goats and hogs had been
suffered to range about, all the young trees had been killed.
Tt appears also from the official records, that the trees were
unexpectedly, some years afterwards, succeeded by a wire
grass which spread over the whole surface. 3 General Beat-
son adds that now this plain " is covered with fine sward, and
is become the finest piece of pasture on the island." The
extent of surface, probably covered by wood at a former
period, is estimated at no less than two thousand acres; at
the present day scarcely a single tree can be found there. It
is also said that in 1709 there were quantities of dead trees
in Sandy Bay ; this place is now so utterly desert, that noth-
ing but so well attested an account could have made me believe
that they could ever have grown there. The fact, that the
goats and hogs destroyed all the young trees as they sprang
up, and that in the course of time the old ones, which were
safe from their attacks, perished from age, seems clearly
made out. Goats were introduced in the year 1502; eighty-
six years afterwards, in the time of Cavendish, it is known
that, they were exceedingly numerous. More than a century
afterwards, in 1731, when the evil was complete and irre-
trievable, an order was issued that all stray animals should
be destroyed. It is very interesting thus to find, that the
arrival of animals at St. Helena in 1501, did not change the
whole aspect of the island, until a period of two hundred
2 It deserves notice, that all the many specimens of this shell found by
me in one spot, differ as a marked variety, from another set of specimens
procured from a different spot.
3 Beatson's St. Helena. Introductory chapter, p. 4.
516 CHARLES DARWIN
and twenty years had elapsed : for the goats were introduced
in 1502, and in 1724 it is said "the old trees had mostly
fallen." There can be little doubt that this great change in
the vegetation affected not only the land-shells, causing eight
species to become extinct, but likewise a multitude of insects.
St. Helena, situated so remote from any continent, in the
midst of a great ocean, and possessing a unique Flo*n, ex-
cites our curiosity. The eight land-shells, though now extinct,
and one living Succinea, are peculiar species found nowhere
else. Mr. Cuming, however, informs me that an English
Helix is common here, its eggs no doubt having been im-
ported in some of the many introduced plants. Mr. Cuming
collected on the coast sixteen species of sea-shells, of which
seven, as far as he knows, are confined to this island. Birds
and insects, 4 as might have been expected, are very few in
number ; indeed I believe all the birds have been introduced
within late years. Partridges and pheasants are tolerably
abundant; the island is much too English not to be subject
to strict game-laws. I was told of a more unjust sacrifice to
4 Among these few insects, I was surprised to find a small Aphodius
(nov. spec.) and an Oryctes, both extremely numerous under dung. When
the island was discovered it certainly possessed no quadruped, excepting
perhaps a mouse: it becomes, therefore, a difficult point to ascertain,
whether these stercovorous insects have since been imported by accident,
or "if aborigines, on what food they formerly subsisted. On the banks of
the Plata, where, from the vast number of cattle and horses, the fine plains
of turf are richly manured, it is vain to seek the many kinds of dung-
feeding beetles, which occur so abundantly in Europe. I observed only an
Oryctes (the insects of this genus in Europe generally^ feed on decayed
vegetable matter) and two species of Phanaeus, common in such situations.
On the opposite side of the Cordillera in Chiloe, another species of Pha-
naeus is exceedingly abundant, and it buries the dung of the cattle in large
earthen balls beneath the ground. There is reason to believe that the
genus Phanaeus, before the introduction of cattle, acted as scavengers to
man. In Europe, beetles, which find support in the matter which has
already contributed towards the life of other and larger animals, are so
numerous that there must be considerably more than one hundred different
species. Considering this, and observing what a quantity of food of this
kind is lost on the plains of La Plata, I imagined I saw an instance where
man had disturbed that chain, by which so many animals are linked
together in their native country. In Van Diemen's Land, however, I
found four species of Onthophagus, two of Aphodius, and one of a third
genus, very abundantly under the dung of cows; yet these latter animals
had been then introduced only thirty-three years. Previously to that time
the kangaroo and some other small animals were the only quadrupeds; and
their dung is of a very different quality from that of their successors intro-
duced by man. In England the greater number of stercovorous beetles
are confined in their appetites; that is, they do not depend indifferently
on any quadruped for the means of subsistence. The change, therefore,
in habits which must have taken place in Van Diemen's Land is highly
remarkable. I am indebted to the Rev. F. W. Hope, who, I hope, will
permit me to call him my master in Entomology, for giving me the names
of the foregoing insects.
THE VOYAGE OF THE BEAGLE 517
such ordinances than I ever heard of even in England. The
poor people formerly used to burn a plant, which grows on the
coast-rocks, and export the soda from its ashes; but a per-
emptory order came out prohibiting this practice, and giving
as a reason that the partridges would have nowhere to build.
In my walks I passed more than once over the grassy plain
bounded by deep valleys, on which Longwood stands.
Viewed from a short distance, it appears like a respectable
gentleman's country-seat. In front there are a few culti-
vated fields, and beyond them the smooth hill of coloured
rocks called the Flagstaff, and the rugged square black mass
of the Barn. On the whole the view was rather bleak and
uninteresting. The only inconvenience I suffered during my
walks was from the impetuous winds. One day I noticed
a curious circumstance ; standing on the edge of a plain, ter-
minated by a great cliff of about a thousand feet in depth,
I saw at the distance of a few yards right to windward, some
tern, struggling against a very strong breeze, whilst, where
I stood, the air was quite calm. Approaching close to the
brink, where the current seemed to be deflected upwards
from the face of the cliff, I stretched out my arm, and
immediately felt the full force of the wind: an invisible
barrier, two yards in width, separated perfectly calm air
from a strong blast.
I so much enjoyed my rambles among the rocks and moun-
tains of St. Helena, that I felt almost sorry on the morning
of the 14th to descend to the town. Before noon I was on
board, and the Beagle made sail.
On the 19th of July we reached Ascension. Those who
have beheld a volcanic island, situated under an arid climate,
will at once be able to picture to themselves the appearance
of Ascension. They will imagine smooth conical hills of a
bright red colour, with their summits generally truncated,
rising separately out of a level surface of black rugged lava.
A principal mound in the centre of the island, seems the
father of the lesser cones. It is called Green Hill: its
name being taken from the faintest tinge of that colour,
which at this time of the year is barely perceptible from the
anchorage. To complete the desolate scene, the black rocks
on the coast are lashed by a wild and turbulent sea.
518 CHARLES DARWIN
The settlement is near the beach; it consists of several
houses and barracks placed irregularly, but well built of
white freestone. The only inhabitants are marines, and some
negroes liberated from slave-ships, who are paid and victu-
alled by government. There is not a private person on the
island. Many of the marines appeared well contented with
their situation; they think it better to serve their one-and-
twenty years on shore, let it be what it may, than in a ship;
in this choice, if I were a marine, I should most heartily
agree.
The next morning I ascended Green Hill, 2840 feet high,
and thence walked across the island to the windward point.
A good cart-road leads from the coast-settlement to the
houses, gardens, and fields, placed near the summit of the
central mountain. On the roadside there are milestones, and
likewise cisterns, where each thirsty passer-by can drink
some good water. Similar care is displayed in each part of the
establishment, and especially in the management of the
springs, so that a single drop of water may not be lost: in-
deed the whole island may be compared to a huge ship kept
in first-rate order. I could not help, when admiring the
active industry, which had created such effects out of such
means, at the same time regretting that it had been wasted on
so poor and trifling an end. M. Lesson has remarked with
justice, that the English nation would have thought of mak-
ing the island of Ascension a productive spot; any other
people would have held it as a mere fortress in the ocean.
Near this coast nothing grows; further inland, an occa-
sional green castor-oil plant, and a few grasshoppers, true
friends of the desert, may be met with. Some grass is scat-
tered over the surface of the central elevated region, and the
whole much resembles the worse parts of the Welsh moun-
tains. But scanty as the pasture appears, about six hundred
sheep, many goats, a few cows and horses, all thrive well on
it. Of native animals, land-crabs and rats swarm in num-
bers. Whether the rat is really indigenous, may well be
doubted ; there are two varieties as described by Mr. Water-
house; one is of a black colour, with fine glossy fur, and
lives on the grassy summit; the other is brown-coloured and
less glossy, with longer hairs, and lives near the settlement
THE VOYAGE OF THE BEAGLE 519
on the coast. Both these varieties are one-third smaller than
the common black rat (M. rattus) ; and they differ from it
both in the colour and character of their fur, but in no
other essential respect. I can hardly doubt that these rats
(like the common mouse, which has also run wild) have
been imported, and, as at the Galapagos, have varied from
the effect of the new conditions to which they have been
exposed: hence the variety on the summit of the island
differs from that on the coast. Of native birds there are
none; but the guinea-fowl, imported from the Cape de
Verd Islands, is abundant, and the common fowl has like-
wise run wild. Some cats, which were originally turned out
to destroy the rats and mice, have increased, so as to be-
come a great plague. The island is entirely without trees,
in which, and in every other respect, it is very far inferior
to St. Helena.
One of my excursions took me towards the S. W. extrem-
ity of the island. The day was clear and hot, and I saw the
island, not smiling with beauty, but staring with naked hide-
ousness. The lava streams are covered with hummocks, and
are rugged to a degree which, geologically speaking, is not
of easy explanation. The intervening spaces are concealed
with layers of pumice, ashes and volcanic tuff. Whilst pass-
ing this end of the island at sea, I could not imagine what
the white patches were with which the whole plain was
mottled; I now found that they were seafowl, sleeping in such
full confidence, that even in midday a man could walk up
and seize hold of them. These birds were the only living
creatures I saw during the whole day. On the beach a great
surf, although the breeze was light, came tumbling over
the broken lava rocks.
The geology of this island is in many respects interesting.
In several places I noticed volcanic bombs, that is, masses of
lava which have been shot through the air whilst fluid, and
have consequently assumed a spherical or pear-shape. Not
only their external form, but, in several cases, their internal
structure shows in a very curious manner that they have re-
volved in their aerial course. The internal structure of one
of these bombs, when broken, is represented very accurately
in the woodcut. The central part is coarsely cellular, the
520
CHARLES DARWIN
cells decreasing in size towards the exterior; where there
is a shell-like case about the third of an inch in thickness,
of compact stone, which again is overlaid by the outside
crust of finely cellular lava. I think there can be little
doubt, first that the external crust cooled rapidly in the state
in which we now see it; secondly, that the still fluid lava
within, was packed by the centrifugal force, generated by
the revolving of the bomb, against the external cooled
crust, and so produced the solid shell of stone; and lastly,
that the centrifugal force, by relieving the pressure in the
more central parts of the bomb, allowed the heated vapours
to expand their cells, thus forming the coarse cellular mass
of the centre. .
A hill, formed of the older series of volcanic rocks, and
which has been incorrectly considered as the crater of a vol-
cano, is remarkable from its broad, slightly hollowed, and
circular summit having been filled up with many successive
layers of ashes and fine scoriae. These saucer-shaped layers
crop out on the margin, forming perfect rings of many dif-
ferent colours, giving to the summit a most fantastic appear-
ance; one of these rings is white and broad, and resembles
THE VOYAGE OF THE BEAGLE 521
a course round which horses have been exercised ; hence the
hill has been called the Devil's Riding School. I brought away
specimens of one of the tufaceous layers of a pinkish colour
and it is a most extraordinary fact, that Professor Ehren-
berg 5 finds it almost wholly composed of matter which has
been organized : he detects in it some siliceous-shielded fresh-
water infusoria, and no less than twenty-five different kinds
of the siliceous tissue of plants, chiefly of grasses. From
the absence of all carbonaceous matter, Professor Ehrenberg
believes that these organic bodies have passed through the
volcanic fire, and have been erupted in the state in which
we now see them. The appearance of the layers induced me
to believe that they had been deposited under water, though
from the extreme dryness of the climate I was forced to im-
agine, that torrents of rain had probably fallen during some
great eruption, and that thus a temporary lake had been
formed into which the ashes fell. But it may now be sus-
pected that the lake was not a temporary one. Anyhow, we
may feel sure, that at some former epoch the climate and
productions of Ascension were very different from what
th^y now are. Where on the face of the earth can we find
a spot, on which close investigation will not discover signs
of that endless cycle of change, to which this earth has been,
is, and will be subjected?
On leaving Ascension, we sailed for Bahia, on the coast
of Brazil, in order to complete the chronometrical measure-
ment of the world. We arrived there on August ist, and
stayed four days, during which I took several long walks.
I was glad to find my enjoyment in tropical scenery had not
decreased from the want of novelty, even in the slightest
degree. The elements of the scenery are so simple, that they
are worth mentioning, as a proof on what trifling circum-
stances exquisite natural beauty depends.
The country may be described as a level plain of about
three hundred feet in elevation, which in all parts has been
worn into flat-bottomed valleys. This structure is remark-
able in a granitic land, but is nearly universal in all those
softer formations of which plains are usually composed.
The whole surface is covered by various kinds of stately
5 Monats. der Konig. Akad. d. Wics. zu Berlin. Vom April, 1845.
522 CHARLES DARWIN
trees, interspersed with patches of cultivated ground, out
of which houses, convents, and chapels arise. It must be
remembered that within the tropics, the wild luxuriance of
nature is not lost even in the vicinity of large cities: for
the natural vegetation of the hedges and hill-sides over-
powers in picturesque effect the artificial labour of man.
Hence, there are only a few spots where the bright red
soil affords a strong contrast with the universal clothing
of green. From the edges of the plain there are distant
views either of the ocean, or of the great Bay with its
low-wooded shores, and on which numerous boats and canoes
show their white sails. Excepting from these points, the
scene is extremely limited; following the level pathways,
on each hand, only glimpses into the wooded valleys below
can be obtained. The houses I may add, and especially the
sacred edifices, are built in a peculiar and rather fantastic
style of architecture. They are all whitewashed; so that
when illumined by the brilliant sun of midday, and as seen
against the pale blue sky of the horizon, they stand out more
like shadows than real buildings.
Such are the elements of the scenery, but it is a hopeless
attempt to paint the general effect. Learned naturalists de-
scribe these scenes of the tropics by naming a multitude of
objects, and mentioning some characteristic feature of each.
To a learned traveller this possibly may communicate some
definite ideas : but who else from seeing a plant in an herba-
rium can imagine its appearance when growing in its native
soil? Who from seeing choice plants in a hothouse, can
magnify some into the dimensions of forest trees, and crowd
others into an entangled jungle? Who when examining in
the cabinet of the entomologist the gay exotic butter-
flies, and singular cicadas, will associate with these lifeless
objects, the ceaseless harsh music of the latter, and the
lazy flight of the former, — the sure accompaniments of the
still, glowing noonday of the tropics? It is when the sun has
attained its greatest height, that such scenes should be
viewed: then the dense splendid foliage of the mango hides
the ground with its darkest shade, whilst the upper branches
are rendered from the profusion of light of the most bril-
liant green. In the temperate zones the case is different — the
THE VOYAGE OF THE BEAGLE 523
vegetation there is not so dark or so rich, and hence the
rays of the declining sun, tinged of a red, purple, or bright
yellow color, add most to the beauties of those climes.
When quietly walking along the shady pathways, and ad-
miring each successive view, I wished to find language to
express my ideas. Epithet after epithet was found too weak
to convey to those who have not visited the intertropical
regions, the sensation of delight which the mind experiences.
I have said that the plants in a hothouse fail to communicate
a just idea of the vegetation, yet I must recur to it. The land
is one great wild, untidy, luxuriant hothouse, made by
Nature for herself, but taken possession of by man, who has
studded it with gay houses and formal gardens. How great
would be the desire in every admirer of nature to behold,
if such were possible, the scenery of another planet ! yet
to every person in Europe, it may be truly said, that at
the distance of only a few degrees from his native soil, the
glories of another world are opened to him. In my last
walk I stopped again and again to gaze on these beauties, and
endeavoured to fix in my mind for ever, an impression which
at the time I knew sooner or later must fail. The form of
the orange-tree, the cocoa-nut, the palm, the mango, the tree-
fern, the banana, will remain clear and separate; but the
thousand beauties which unite these into one perfect scene
must fade away; yet they will leave, like a tale heard in
childhood, a picture full of indistinct, but most beautiful
figures.
August 6th. — In the afternoon we stood out to sea, with
the intention of making a direct course to the Cape de Verd
Islands. Unfavourable winds, however, delayed us, and on
the 12th we ran into Pernambuco, — a large city on the
coast of Brazil, in latitude 8° south. We anchored outside
the reef; but in a short time a pilot came on board and
took us into the inner harbour, where we lay close to the
town.
Pernambuco is built on some narrow and low sand-banks,
which are separated from each other by shoal channels of
salt water. The three parts of the town are connected to-
gether by two long bridges built on wooden piles. The
town is in all parts disgusting, the streets being narrow, ill-
524 CHARLES DARWIN
paved, and filthy; the houses, tall and gloomy. The season
of heavy rains had hardly come to an end, and hence the
surrounding country, which is scarcely raised above the
level of the sea, was flooded with water; and I failed in
all my attempts to take walks.
The flat swampy land on which Pernambuco stands is sur-
rounded, at the distance of a few miles, by a semicircle of
low hills, or rather by the edge of a country elevated per-
haps two hundred feet above the sea. The old city of
Olinda stands on one extremity of this range. One day I
took a canoe, and proceeded up one of the channels to visit
it; I found the old town from its situation both sweeter and
cleaner than that of Pernambuco. I must here commemorate
what happened for the first time during our nearly five
years' wandering, namely, having met with a want of polite-
ness. I was refused in a sullen manner at two different
houses, and obtained with difficulty from a third, per-
mission to pass through their gardens to an uncultivated hill,
for the purpose of viewing the country. I feel glad that
this happened in the land of the Brazilians, for I bear
them no good will — a land also of slavery, and therefore
of moral debasement. A Spaniard would have felt ashamed
at the very thought of refusing such a request, or of
behaving to a stranger with rudeness. The channel by which
we went to and returned from Olinda, was bordered on each
side by mangroves, which sprang like a miniature forest out
of the greasy mud-banks. The bright green colour of these
bushes always reminded me of the rank grass in a church-
yard : both are nourished by putrid exhalations ; the one
speaks of death past, and the other too often of death
to come.
The most curious object which I saw in this neighbour-
hood, was the reef that forms the harbour. I doubt whether
in the whole world any other natural structure has so arti-
ficial an appearance. 6 It runs for a length of several miles in
an absolutely straight line, parallel to, and not far distant
from, the shore. It varies in width from thirty to sixty
yards, and its surface is level and smooth ; it is composed of
6 I have described this Bar in detail, in the Lond. and Edin. Phil. Mag,,
vol. xix. (1841), p. 257.
THE VOYAGE OF THE BEAGLE 525
obscurely stratified hard sandstone. At high water the waves
break over it; at low water its summit is left dry, and it
might then be mistaken for a breakwater erected by Cyclo-
pean workmen. On this coast the currents of the sea tend
to throw up in front of the land, long spits and bars of
loose sand, and on one of these, part of the town of Per-
nambuco stands. In former times a long spit of this nature
seems to have become consolidated by the percolation of
calcareous matter, and afterwards to have been gradually
upheaved; the outer and loose parts during this process hav-
ing been worn away by the action of the sea, and the solid
nucleus left as we now see it. Although night and day the
waves of the open Atlantic, turbid with sediment, are
driven against the steep outside edges of this wall of stone,
yet the oldest pilots know of no tradition of any change in its
appearance. This durability is much the most curious fact
in its history : it is due to a tough layer, a few inches thick,
of calcareous matter, wholly formed by the successive
growth and death of the small shells of Serpulse, together
with some few barnacles and nulliporae. These nulliporse,
which are hard, very simply-organized sea-plants, play an
analogous and important part in protecting the upper sur-
faces of coral-reefs, behind and within the breakers, where
the true corals, during the outward growth of the mass,
become killed by exposure to the sun and air. These in-
significant organic beings, especially the Serpulse, have done
good service to the people of Pernambuco; for without their
protective aid the bar of sandstone would inevitably have
been long ago worn away and without the bar, there would
have been no harbour.
On the 19th of August we finally left the shores of Brazil.
I thank God, I shall never again visit a slave-country. To
this day, if I hear a distant scream, it recalls with painful
vividness my feelings, when passing a house near Pernam-
buco, I heard the most pitiable moans, and could not but
suspect that some poor slave was being tortured, yet knew
that I was as powerless as a child even to remonstrate. I sus-
pected that these moans were from a tortured slave, for I
was told that this was the case in another instance. Near
Rio de Janeiro I lived opposite to an old lady, who kept
526 CHARLES DARWIN
screws to crush the fingers of her female slaves, I have
stayed in a house where a young household mulatto, daily
and hourly, was reviled, beaten, and persecuted enough to
break the spirit of the lowest animal. I have seen a little
boy, six or seven years old, struck thrice with a horse-whip
(before I could interfere) on his naked head, for having
handed me a glass of water not quite clean; I saw his
father tremble at a mere glance from his master's eye.
These latter cruelties were witnessed by me in a Spanish
colony, in which it has always been said, that slaves are
better treated than by the Portuguese, English, or other
European nations. I have seen at Rio de Janeiro a powerful
negro afraid to ward off a blow directed, as he thought, at his
face. I was present when a kind-hearted man was on the
point of separating forever the men, women, and little
children of a large number of families who had long lived
together. I will not even allude to the many heart-sickening
atrocities which I authentically heard of; — nor would I have
mentioned the above revolting details, had I not met with sev-
eral people, so blinded by the constitutional gaiety of the negro
as to speak of slavery as a tolerable evil. Such people have
generally visited at the houses of the upper classes, where
the domestic slaves are usually well treated; and they have
not, like myself, lived amongst the lower classes. Such
inquirers will ask slaves about their condition; they forget
that the slave must indeed be dull, who does not calculate
on the chance of his answer reaching his master's ears.
It is argued that self-interest will prevent excessive cru-
elty ; as if self-interest protected our domestic animals, which
are far less likely than degraded slaves, to stir up the rage
of their savage masters. It is an argument long since pro-
tested against with noble feeling, and strikingly exemplified,
by the ever-illustrious Humboldt. It is often attempted to
palliate slavery by comparing the state of slaves with our
poorer countrymen: if the misery of our poor be caused
not by the laws of nature, but by our institutions, great is
our sin ; but how this bears on slavery, I cannot see ; as well
might the use of the thumb-screw be defended in one
land, by showing that men in another land suffered from
some dreadful disease. Those who look tenderlv at the slave
THE VOYAGE OF THE BEAGLE 527
owner, and with a cold heart at the slave, never seem to put
themselves into the position of the latter; what a cheerless
prospect, with not even a hope of change ! picture to your-
self the chance, ever hanging over you, of your wife and
your little children — those objects which nature urges even
the slave to call his own — being torn from you and sold
like beasts to the first bidder ! And these deeds are done
and palliated by men, who profess to love their neighbours
as themselves, who believe in God, and pray that his Will be
done on earth ! It makes one's blood boil, yet heart tremble,
to think that we Englishmen and our American descendants,
with their boastful cry of liberty, have been and are so
guilty : but it is a consolation to reflect, that we at least have
made a greater sacrifice, than ever made by any nation,
to expiate our sin.
On the last day of August we anchored for the second time
at Porto Praya in the Cape de Verd archipelago ; thence we
proceeded to the Azores, where we stayed six days. On the
2nd of October we made the shores of England ; and at Fal-
mouth I left the Beagle, having lived on board the good little
vessel nearly five years.
Our Voyage having come to an end, I will take a short
retrospect of the advantages and disadvantages, the pains
and pleasures, of our circumnavigation of the world. If a
person asked my advice, before undertaking a long voyage,
my answer would depend upon his possessing a decided taste
for some branch of knowledge, which could by this means be
advanced. No doubt it is a high satisfaction to behold various
countries and the many races of mankind, but the pleasures
gained at the time do not counterbalance the evils. It is
necessary to look forward to a harvest, however distant
that may be, when some fruit will be reaped, some good
effected.
Many of the losses which must be experienced are obvious ;
such as that of the society of every old friend, and of the
sight of those places with which every dearest remembrance
is so intimately connected. These losses, however, are at
the time partly relieved by the exhaustless delight of antici-
528 CHARLES DARWIN
pating the long wished-for day of return. If, as poets say,
life is a dream, I am sure in a voyage these are the visions
which best serve to pass away the long night. Other losses,
although not at first felt, tell heavily after a period: these
are the want of room, of seclusion, of rest; the jading feel-
ing of constant hurry ; the privation of small luxuries, the loss
of domestic society and even of music and the other pleasures
of imagination. When such trifles are mentioned, it is
evident that the real grievances, excepting from accidents, of
a sea-life are at an end. The short space of sixty years has
made an astonishing difference in the facility of distant
navigation. Even in the time of Cook, a man who left
his fireside for such expeditions underwent severe privations.
A yacht now, with every luxury of life, can circumnavigate
the globe. Besides the vast improvements in ships and
naval resources, the whole western shores of America are
thrown open, and Australia has become the capital of a
rising continent. How different are the circumstances to a
man shipwrecked at the present day in the Pacific, to what
they were in the time of Cook ! Since his voyage a hemi-
sphere has been added to the civilized world.
If a person suffer much from sea-sickness, let him weigh
it heavily in the balance. I speak from experience: it is no
trifling evil, cured in a week. If, on the other hand, he take
pleasure in naval tactics, he will assuredly have full scope
for his taste. But it must be borne in mind, how large a
proportion of the time, during a long voyage, is spent on
the water, as compared with the days in harbour. And what
are the boasted glories of the illimitable ocean. A tedious
waste, a desert of water, as the Arabian calls it. No doubt
there are some delightful scenes. A moonlight night, with
the clear heavens and the dark glittering sea, and the white
sails filled by the soft air of a gently blowing trade-wind, a
dead calm, with the heaving surface polished like a mirror,
and all still except the occasional flapping of the canvas.
It is well once to behold a squall with its rising arch and
coming fury, or the heavy gale of wind and mountainous
waves. I confess, however, my imagination had painted
something more grand, more terrific in the full-grown storm.
It is an incomparably finer spectacle when beheld on shore,
THE VOYAGE OF THE BEAGLE 529
where the waving trees, the wild flight of the birds, the
dark shadows and bright lights, the rushing of the torrents
all proclaim the strife of the unloosed elements. At sea
the albatross and little petrel fly as if the storm were their
proper sphere, the water rises and sinks as if fulfilling its
usual task, the ship alone and its inhabitants seem the objects
of wrath. On a forlorn and weather-beaten coast, the scene
is indeed different, but the feelings partake more of horror
than of wild delight.
Let us now look at the brighter side of the past time. The
pleasure derived from beholding the scenery and the general
aspect of the various countries we have visited, has decidedly
been the most constant and highest source of enjoyment. It
is probable that the picturesque beauty of many parts of Eu-
rope exceeds anything which we beheld. But there is a
growing pleasure in comparing the character of the scenery
in different countries, which to a certain degree is distinct
from merely admiring its beauty. It depends chiefly on an
acquaintance with the individual parts of each view. I am
strongly induced to believe that as in music, the person who
understands every note will, if he also possesses a proper
taste, more thoroughly enjoy the whole, so he who examines
each part of a fine view, may also thoroughly comprehend
the full and combined effect. Hence, a traveller should be
a botanist, for in all views plants form the chief embellish-
ment. Group masses of naked rock, even in the wildest
forms, and they may for a time afford a sublime spectacle,
but they will soon grow monotonous. Paint them with bright
and varied colours, as in Northern Chile, they will become
fantastic; clothe them with vegetation, they must form a
decent, if not a beautiful picture.
When I say that the scenery of parts of Europe is probably
superior to anything which we beheld, I except, as a class by
itself, that of the intertropical zones. The two classes cannot
be compared together; but I have already often enlarged on
the grandeur of those regions. As the force of impressions
generally depends on preconceived ideas, I may add, that
mine were taken from the vivid descriptions in the Personal
Narrative of Humboldt, which far exceed in merit anything
else which I have read. Yet with these high-wrought ideas,
530 CHARLES DARWIN
my feelings were far from partaking of a tinge of disappoint-
ment on my first and final landing on the shores of Brazil.
Among the scenes which are deeply impressed on my mind,
none exceed in sublimity the primeval forests undefaced by
the hand of man ; whether those of Brazil, where the powers
of Life are predominant, or those of Tierra del Fuego,
where Death and Decay prevail. Both are temples filled with
the varied productions of the God of Nature: — no one can
stand in these solitudes unmoved, and not feel that there is
more in man than the mere breath of his body. In calling
up images of the past, I find that the plains of Patagonia
frequently cross before my eyes; yet these plains are pro-
nounced by all wretched and useless. They can be described
only by negative characters; without habitations, without
water, without trees, without mountains, they support merely
a few dwarf plants. Why, then, and the case is not peculiar
to myself, have these arid wastes taken so firm a hold on
my memory ? Why have not the still more level, the greener
and more fertile Pampas, which are serviceable to mankind,
produced an equal impression? I can scarcely analyze these
feelings : but it must be partly owing to the free scope given
to the imagination. The plains of Patagonia are boundless,
for they are scarcely passable, and hence unknown: they
bear the stamp of having lasted, as they are now, for ages,
and there appears no limit to their duration through future
time. If, as the ancients supposed, the flat earth was sur-
rounded by an impassable breadth of water, or by deserts
heated to an intolerable excess, who would not look at these
last boundaries to man's knowledge with deep but ill-defined
sensations ?
Lastly, of natural scenery, the views from lofty mountains,
through certainly in one sense not beautiful, are very memo-
rable. When looking down from the highest crest of the
Cordillera, the mind, undisturbed by minute details, was
filled with the stupendous dimensions of the surrounding
masses.
Of individual objects, perhaps nothing is more certain to
create astonishment than the first sight in his native haunt o£
a barbarian — of man in his lowest and most savage state.
One's mind hurries back over past centuries, and then asks,
THE VOYAGE OF THE BEAGLE 531
could our progenitors have been men like these? — men,
whose very signs and expressions are less intelligible to us
than those of the domesticated animals; men, who do not
possess the instinct of those animals, nor yet appear to boast
of human reason, or at least of arts consequent on that
reason. I do not believe it is possible to describe or paint
the difference between savage and civilized man. It is
the difference between a wild and tame animal: and part
of the interest in beholding a savage, is the same which
would lead every one to desire to see the lion in his desert,
the tiger tearing his prey in the jungle, or the rhinoceros
wandering over the wild plains of Africa.
Among the other most remarkable spectacles which we
have beheld, may be ranked, the Southern Cross, the cloud
of Magellan, and the other constellations of the southern
hemisphere — the water-spout — the glacier leading its blue
stream of ice, over-hanging the sea in a bold precipice — a
lagoon-island raised by the reef-building corals — an active
volcano — and the overwhelming effects of a violent earth-
quake. These latter phenomena, perhaps, possess for me a
peculiar interest, from their intimate connection with the
geological structure of the world. The earthquake, however,
must be to every one a most impressive event: the earth,
considered from our earliest childhood as the type of solid-
ity, has oscillated like a thin crust beneath our feet; and
in seeing the laboured works of man in a moment over-
thrown, we feel the insignificance of his boasted power.
It has been said, that the love of the chase is an inherent
delight in man — a relic of an instinctive passion. If so, I
am sure the pleasure of living in the open air, with the sky
for a roof and the ground for a table, is part of the same
feeling; it is the savage returning to his wild and native
habits. I always look back to our boat cruises, and my land
journeys, when through unfrequented countries, with an ex-
treme delight, which no scenes of civilization could have
created. I do not doubt that every traveller must remember
the glowing sense of happiness which he experienced, when
he first breathed in a foreign clime, where the civilized man
had seldom or never trod.
There are several other sources of enjoyment in a long
532 CHARLES DARWIN
voyage, which are of a more reasonable nature. The map
of the world ceases to be a blank ; it becomes a picture full
of the most varied and animated figures. Each part assumes
its proper dimensions: continents are not looked at in the
light of islands, or islands considered as mere specks, which
are, in truth, larger than many kingdoms of Europe. Africa,
or North and South America, are well-sounding names, and
easily pronounced; but it is not until having sailed for
weeks along small portions of their shores, that one is thor-
oughly convinced what vast spaces on our immense world
these names imply.
From seeing the present state, it is impossible not to look
forward with high expectations to the future progress of
nearly an entire hemisphere. The march of improvement,
consequent on the introduction of Christianity throughout
the South Sea, probably stands by itself in the records of
history. It is the more striking when we remember that only
sixty years since, Cook, whose excellent judgment none will
dispute, could foresee no prospect of a change. Yet these
changes have now been effected by the philanthropic spirit
of the British nation.
In the same quarter of the globe Australia is rising, or
indeed may be said to have risen, into a grand centre of
civilization, which, at some not very remote period, will rule
as empress over the southern hemisphere. It is impossible
for an Englishman to behold these distant colonies, without
a high pride and satisfaction. To hoist the British flag,
seems to draw with it as a certain consequence, wealth, pros-
perity, and civilization.
In conclusion, it appears to me that nothing can be more
improving to a young naturalist, than a journey in distant
countries. It both sharpens, and partly allays that want and
craving, which, as Sir J. Herschel remarks, a man experi-
ences although every corporeal sense be fully satisfied. The
excitement from the novelty of objects, and the chance of
success, stimulate him to increased activity. Moreover, as a
number of isolated facts soon become uninteresting, the
habit of comparison leads to generalization. On the other
hand, as the traveller stays but a short time in each place,
his descriptions must generally consist of mere sketches, in-
THE VOYAGE OF THE BEAGLE 533
stead of detailed observations. Hence arises, as I have found
to my cost, a constant tendency to fill up the wide gaps of
knowledge, by inaccurate and superficial hypotheses.
But I have too deeply enjoyed the voyage, not to recom-
mend any naturalist, although he must not expect to be so
fortunate in his companions as I have been, to take all
chances, and to start, on travels by land if possible, if other-
wise, on a long voyage. He may feel assured, he will meet
with no difficulties or dangers, excepting in rare cases, nearly
so bad as he beforehand anticipates. In a moral point of
view, the effect ought to be, to teach him good-humoured
patience, freedom from selfishness, the habit of acting for
himself, and of making the best of every occurrence. In
short, he ought to partake of the characteristic qualities of
most sailors. Travelling ought also to teach him distrust-;
but at the same time he will discover, how many truly kind-
hearted people there are, with whom he never before had,
or ever again will have any further communication, who
yet are ready to offer him the most disinterested assistance.
INDEX
INDEX
Abbott, Mr., on spiders, 46.
Aborigines banished from Van Die-
men's Land, 471.
of Australia, 459-474.
Abrolhos, 24.
Absence of trees in Pampas, 56.
Aconcagua, volcano of, 269, 309.
Actinia, stinging species, 489.
Africa, Southern part desert, yet
supports large animals, 97.
Agouti, habits of, 81.
Ague common in Peru, 386.
Albemarle Island, 398.
Allan, Dr., on Diodon, 24.
on Holuthuriae, 490.
Alluvium, # saliferous, in Peru, 384.
stratified, in Andes, 334.
Amblyrhynchus, 408, 418.
Anas, species of, 214.
Animalculae, see Infusoria.
Antarctic islands, 264.
Antipodes, 440.
Ants at Keeling Island, 481.
— in Brazil, 45.
Apires, or miners, 361.
Aplysia, 16.
Apple-trees 316.
Aptenodytes demersa, 214.
Areas of alternate movements in the
Pacific and Indian oceans, 506.
Armadilloejs, habits of, 108.
, fossil animal allied to, 142,
169.
Arrow-heads, ancient, 377.
Ascension, 517.
Aspalax, blindness of, 62.
Athene, 81, 138.
Atolls, 491.
Attagis, 106.
Atwater, Mr., on the prairies, 131.
Audubon, M., on smelfing-power of
carrion hawks, 198.
Australia, 457.
Australian barrier, 498.
Azara on spiders, 46.
on rain in La Plata, 57.
on range of carrion-hawks, 69.
on habits of carrion-hawks, 67.
on a thunder-storm, 72.
on ostrich-eggs, 103.
on bows and arrows, 117.
■ on new plants springing up,
131.
on great droughts, 145,
on hydrophobia, 374.
Bachman, Mr., on carrion-hawks,
199.
Bahia Blanca, 85-117.
Bahia, Brazil, 22.
, scenery of, 520.
Balbi on coral reefs, 495.
Bald Head, Australia, 474.
Ballenar, Chile, 369.
Banda Oriental, 155.
Banks's Hill, 225.
Barking-bird, 306.
Basaltic platform of Santa Cruz,
194.
Bathurst, Australia, 466.
Bats, vampire, 32.
Bay of Islands, New Zealand, 441.
Beads', hill of, 162.
Beagle Channel, Tierra del Fuego,
233.
Beech-trees, 251, 298.
Beetles alive in sea, 172.
, dung-feeders, 516.
at St. Julian, 184.
in brackish water, 32.
on a fungus, 41.
Behring's Straits, fossils of, 145.
Bell of Quillota, 271.
Benchuca, 349.
Berkeley Sound, 202.
, Rev. J., on Conferva, 25.
, on Cyttaria, 252.
Bibron, M., 404, 409.
Bien-te-veo, 65.
Birds of the Galapagos Archipelago,
401, 418.
, tameness of, 422.
Birgos latro, 488.
Bizcacha, habits of, 81, 136.
Blackwall, Mr., on Spiders, 175.
Blindness of tucutuco, 62.
Body, frozen, 100, 265.
Bolabola, 494, 499.
Bolas, manner of using, 55, 123.
Bombs, volcanic, 520.
Bones of the guanaco collected in
certain spots, 181.
, fire made of, 209.
, fossil, 91, 139, 142, 168, 186.
, recent in Pampas, 146.
Bory St. Vincent on frogs, 404.
Boulders, 201, 264.
Bramador, El, 382.
Brazil, great area of granite, 22.
Breaches in coral reefs. 502.
Breakwater of sea-weea, 256.
537
538
INDEX
Brewster, Sir D., on a calcareous
deposit, 20.
Bridge of hide, 279.
of Incas, 354, 377.
Buckland, Dr., on fossils, 144.
Buenos Ayres, 133.
Buffon on American animals, 187.
Bug of Pampas, 349.
Buildings, Indian, Z77^ 389.
Bulimus on desert places, 368.
Burchell, Mr., on food of quadru-
peds, 99.
, on ostrich eggs, 103.
, on perforated stones, 284.
Butterflies, flocks of, 172.
Butterfly producing clicking sound,
44-
Button, Jemmy, 222.
Byron's account of fox of Falk-
lands, 208.
Byron on an Indian killing his
child, 231.
Cacti, 179, 277, 396.
Cactornis, 401, 418.
Calcareous casts of branches and
roots of trees at King George's
Sound, 475.
Calosoma on wing out at sea, 172.
■ incrustations on rocks of As-
cension, 20.
Callao, 386.
Calodera, 137.
Calomys bizcacha, 136.
Camarhynchus, 402, 418.
Camelidae, fossil animal allied to,
186.
Canis antarcticus, 208.
fulvipes, 297.
Capybara, or carpincho, 60, 305.
fossil allied to, 94.
Cape Horn, 226.
of Good Hope, 97.
Caracara, or Carrancha, 66.
Cardoon, beds of, 131, 161.
Carmichael, Cnpt., 424.
Carrion-hawks, 66 y 132, 198.
Casarita, 107.
Castro, Chiloe, 295, 313.
Casts of trees, 474.
Casuchas, 355.
Cathartes, 69, 199/302.
Cats run wild, 132, 519.
good to eat, 128.
scratch trees, 148.
cruelty to mice, 214.
Cattle, effects of their grazing on
the vegetation, 130.
killed by great droughts, 145,
160.
know each other, 158.
, curious breed of, 158.
. waste of, 162.
wild at the Falkland Islands,
205, 206.
Cauquenes, hot springs of, 280.
Causes of extinction of species among
mammalia, 188.
of discoloured sea, 26.
Cavia Patagonica, 81.
Cervus campestris, 59.
Ceryle Americana, 151.
Chacao, Chiloe, 292.
Chagos, atolls, 504.
Chalk-like mud, 490.
Chamisso on drifted seeds and trees,
480, 487.
on coral reefs, 492.
Changes in vegetation of Pampas,
131.
of St. Helena, 516.
Charles Island, Galapagos Archi-
pelago, 397.
Cheese, salt required for, 77.
Cheucau, 296, 305.
Chile, 269, 357.
, features of country, 271.
Chiloe, 291.
, forests of, and climate, 260.
, roads of, 291, 310.
, inhabitants of, 290, 295.
Chionis, 106.
Chonos, Archipelago, 298.
, climate of, 260.
, ornithology of, 305.
Chupat, Rio, 119.
Cladonia, 384.
Clearness of atmosphere within An-
des, in Chile, 273.
Climate of Tierra del Fuego and
Falkland Islands, 259.
Antarctic Islands, 264.
Galapagos, 394, 399-
, change of, in Chile, 378.
Clouds of vapour after rain, 34.
on Corcovado, 39.
hanging low, 388.
hanging low at sea, 425.
Coleoptera in Tropics, 44.
out at sea, 173.
of St. Julian, 184.
Colias edusa, flocks of, 172.
Colnett, Capt., on spawn in sea, 27,
, on a marine lizard, 408.
, on transport of seeds, 415.
Colonia del Sacramiento, 157.
Colorado, Rio, 82.
Compound animals, 216.
Concepcion, Chile, 321.
Condor, habits of, 196, 200, 287.
Confervae, pelagic, 25.
Conglomerate on the Ventana, 121.
in Cordillera, 338, 339.
Conurus, 151.
Convicts of Mauritius, 510.
, condition of, in New South
Wales, 469.
Cook, Capt., on Kelp, 255.
Copiapo, river and valley of, 371.
, town of, 375.
Coquimbo, 364.
Coral formations, 425, 477-509.
, stinging species of, 489.
INDEX
539
Coral, dead, 486, 505.
Corallines, 216.
Corcov,ado, clouds on, 39.
volcano, 309.
Cordillera, appearance of, 274, 293,
338.
-, different productions on east
and west side, 346.
, passage of, 334.
« , structure of valleys, 335.
, geology of, 339, 35 1.
-, rivers of, 336.
, of Copiapo, 382.
Cormorant catching fish, 213.
Corral, where animals are slaugh-
tered at Buenos Ayres, 134.
Coseguina, eruption of, 309.
Countries, unhealthy, 386.
Couthouy, Mr., on coral-reefs, 500.
Crabs, hermit species of, 482.
at Keeling Island, 488.
at St. Paul's, 20.
Craters, number of, at the Gala-
pagos Archipelago, 394.
■ of elevation, 511.
Crisia, 216.
Cruelty to animals, 168.
Crustacea, pelagic, 175.
Ctenomys Brasiliensis, 61.
, fossil species of, 94.
Cucao, Chiloe, 312.
Cuckoo-like habits of Molothrus, 63.
Cuentas, Sierra de, 162.
Cumbre of Cordillera, 355.
Cuming, Mr., on shells, 414, 516.
Cuttle-fish, habits of, 17.
Cuvier on Diodon, 24.
Cynara, mi.
Cyttaria Darwinii, 252.
Dacelo Iagoensis, 12.
Dasypus, three species of, 108.
Deer, 59,. 145.
Degradation of tertiary formations,
364.
Deinornis, 451.
Deserts, 369, 384.
Desmodus, 32.
Despoblado, valley of, 376.
Dieffenbach on Auckland Island,
260, 460.
Diodon, habits of, 23.
Discoloured sea, 24.
Diseases from miasma, 386, 460.
Distribution of mammalia in Amer-
ica, 143. #
of animals on opposite sides of
Cordilleras, 346.
— of frogs, 404.
of fauna of Galapagos, 417.
Dobrizhoffer on ostriches, 105.
on a hail-storm, 128.
Docks, imported, 452.
Dogs, shepherd, 163.
D'Orbigny, Travels in South Amer-
ica, 90, 105, 132, 142, 163, 181.
Doris, eggs of, 215.
Doubleday, Mr., on a noise made by
the butterfly, 44.
Drigg, lightning tubes at, 70.
Droughts, great, in Pampas, 145.
Dryness of St. J ago, 14.
of winds in Tierra del Fuego,
247-
of air in Cordillera, 345.
Du Bois, 404, 423.
Dung-feeding beetles, 516.
Dust falling from atmosphere, 15.
Earthenware fossil, 391.
Earthquake, accompanied by an ele-
vation of the coast, 329.
■ accompanied by rain, 373.
at Callao, 390.
at Concepcion, 321.
at Coquimbo, 362.
at Keeling and Vanikoro, and
Society Islands, 500, 501.
— — at Valdivia, 320.
, causes of, 330.
, effect of, on springs, 271.
, effect of, on bottom of sea,
325
, effects of, on rocks, 274, 320.
effects of, on sea, 312, 320,
3*3>
effects of, on a river-bed, 379.
— , line of vibration, 325.
■ on S. A. coast, 262.
, tossing fragments from the
ground, 213.
, twisting movement of, 326,
327-
Eggs of Doris, 215.
Ehrenberg, Prof., on Atlantic dust,
15.
on infusoria in Pampas, 94,
142.
176.
on infusoria in the open sea,
237-
on infusoria in Patagonia, 185.
on infusoria in Fuegian paint,
r.
on Infusoria in coral mud, 490.
on infusoria in tuff at Ascen-
sion, 521.
— on phosphorescence of the sea,
177.
on noises from a hill, 382.
Eimeo, view of, 429.
Elater, springing powers of, 41.
Electricity of atmosphere within
Andes, 345.
Elephant, weight of, 99.
Elevated shells, 96, 143, 184, 270,
316, 329, 364, 39i.
Elevation of coasts of Chile, 271,
316, 326, 328, 358, 365, 378
)f B.
ot a. Blanca, 91.
of Patagonia, 186, 392.
of Pampas, 142.
of mountain-chains, 328.
of Cordillera, 335, 339, 35'
of fringing-reefs, 503.
540
INDEX
Elevation of the coast of Peru, 391.
within human period, 392.
Entomology of the Galapagos Archi-
pelago, 404, 414, 416.
of Brazil, 43.
« of Patagonia, 184, 346.
of Tierra del Fuego, 254.
of Keeling Island, 481.
of St. Helena, 516.
Entre Rios, geology of, 141.
Epeira, habits of, 46.
Erratic blocks, how transported, 264.
absent in intertropical coun-
tries, 264.
- on plains of Santa Cruz, 201.
of Tierra del Fuego, 264.
Estancia, value of, 158.
Extermination of species and races,
187, 458, 472.
Extinction of shells at St. Helena,
5i4-
of species, causes of, 187, 188.
of man in New South Wales,
458, 472.
Eyes of tucutuco and mole, 63.
Falconer, Dr., on the Sivatherium,
150.
, Jesuit, on the Indians, 116.
, Jesuit, on rivers in Pampas,
119.
Jesuit, on natural enclosures,
128.
Falkland Islands, 202.
, birds tame at, 422.
, absence of trees at, 58.
, carrion-hawks of, 68.
, wild cattle and horses of, 204.
, climate of, 258.
, peat of, 304.
Fat, quantity eaten, 130.
Fear, an acquired instinct, 423.
Februa, 44.
Fennel, run wild, 132.
Ferguson, Dr., on miasma, 387.
Fern-trees, 261, 473.
Fernando Noronha, 21, 396.
Fields of dead coral, 485.
Fire, art of making, 209, 433.
Fish, eating coral, 490.
of Galapagos, 414.
— ■ — emitting harsh sound, 149.
Flamingoes, 78.
Fleas, 366.
Floods after droughts, 147.
clear after snow, 338.
Flora of the Galapagos, 396, 415,
418.
of Keeling Island, 479.
of St. Helena, 513.
Flustraceae, 216.
Forests, absence of, in La Plata, 58.
01 Tierra del Fuego, 225, 258,
303.
of Chiloe, 259, 297, 302, 310.
of Valdivia, 315, 318.
1 of New Zealand, 451.
Forests of Australia, 457.
Fossil Mammalia, 93, 139, 142, 168,
186.
earthenware, 392.
Fox of the Falkland Islands, 208.
of Chiloe, 297.
Friendly Archipelago, 506.
Frogs, noises of, 39.
, bladders of, 406.
and toads, not found on oceanic
islands, 405.
Frozen soil, 100, 263.
Fruit-trees, southern limit of, 260.
Fucus giganteus, 255.
Fuegians, 219-251.
Fulgurites, 70.
Fungus, edible, 252.
Furnarius, 107.
Galapagos Archipelago, 394; natural
history of, 400.
belongs to American Zoology,
400, 416.
Gale of wind, 232, 299.
Gallegos River, fossil bones at, 186.
Gallinazo, 66.
Gauchos, S3, 166.
, character of, 170.
live on meat, 129.
Gay, M., on floating islands, 282.
, on shells in brackish water, 32.
Geese at the Falkland Islands, 214.
Geographical distribution of Ameri-
can animals, 144, 346.
of frogs, 404.
of fauna of Galapagos, 416.
Geology of Cordillera, 338, 351.
of Patagonia, 184, 195.
of St. Jago, 16.
of St. Paul, 18.
of B. Blanca, 93.
of Pampas, 141.
of Brazil, 22.
Georgia, climate of, 265.
Geospiza, 401, 418.
Gill, Mr., on an upheaved river-
bed, 379.
Gillies, Dr., on the Cordillera, 342.
Glaciers in Tierra del Fuego, 240,
261.
in Cordillera, 344.
in lat. 46 ° 40', 263.
Glowworms, 40.
Goats, destructive to vegetation at
St. Helena, 515.
, bones of, 182,
Goitre, 333.
Gold-washing, 283.
Good Success Bay, 219.
Gossamer spider, 173.
Gould, Mr., on the Calodera, 137.
, on birds of Galapagos, 401.
Granite mountains, Tres Montes,
301.
of Cordillera, 339.
Graspus, 20.
Gravel, how far transported, 120.
INDEX
541
Gravel of Patagonia, 86, 185.
Greenstone, fragments of, 274.
Gryllus migratorius, 349.
Guanaco, habits of, 179.
, fossil allied genus, 187.
Guantajaya, mines of, 384.
Guardia del Monte, 130.
Guasco, 367.
Guasos of Chile, 275.
Guava, imported into Tahiti, 426.
Guinea-fowl, 14, 520.
Gunnera scabra, 297.
Gypsum, great beds of, 339.
in salt-lake, 77.
in Patagonian tertiary-beds,
185.
at Iquique with salt, 384.
- at Lima with shells, 390.
Hachette, M., on lightning-tubes, 71.
Hailstorm, 128.
Hall, Capt. Basil, on terraces of
Coquimbo, 363.
Hare, Varying, 56.
Head, Capt., on thistle-beds, 132,
136.
Height of snow-line on Cordillera,
261.
Henslow, Prof., on potatoes, 303.
on plants of Keeling Island,
479.
Hermit crabs, 482.
Hill, emitting a noise, 382.
Himantopus, 126.
Hogoleu barrier-reef, 495.
Holes made by a bird, 107.
Holman on drifted seeds, 479.
Holuthurise feeding on coral, 490.
Hooker, Sir J., on the Cardoon, 132.
, Dr. J. D., on the Kelp, 255.
, Dr. J. D., on Gafapageian
plants, 41 s, 419.
Horn, Cane, 226.
Horner, Mr., on a calcareous de-
posit, 20.
Horse, powers of swimming of, 156.
, wild at the Falkland Islands,
206.
fossil, 94, 142.
Horsefly, 184.
Horsemanship of the Gauchos, 165,
210.
Horses difficult to drive, 123.
drop excrement on paths, 131.
killed by great droughts, 148.
, multiplication of, 248.
broken in, 165.
Hot springs of Cauquenes, 280.
Huacas, 389, 391.
Humboldt on burnished rocks, 23.
on the atmosphere in tropics,
42.
on frozen soil, 100.
- on hybernation, in.
on potatoes, 303.
on earthquakes and rain, 373.
- on miasma, 387, 460.
Humming-birds of Rio de Janeiro,
42.
of Chile, 291.
Hybernation of animals, HI.
Hydrochaerus capybara, 60.
Hydrophobia, 374.
Hyla, 39.
Hymenophallus, 43.
Ibis melanops, 179.
Ice prismatic structure of, 344.
Icebergs, 201, 240, 263-268.
Incas Bridge, 355, 377.
Incrustations on coast rocks, 19, 22,
Indian fossil remains, 392.
Indians, attacks of, 75, 87.
1 Patagonians, 248.
, Araucarians, 317.
of the Pampas, 114.
of Valdivia, 317.
, perforated stones used by, 284.
powers of tracking, 347.
, grave of, 183, 201.
, ruins of houses of, in Cordil-
lera, 37,7> .3?9. „
, antiquities of, in La Plata, 56,
117.
decrease in numbers, 116.
Infection, 459.
Infusoria in dust of the Atlantic, 15.
■ in the sea, 26, 176.
■ in Pampas, 94, 142.
in Patagonia, 185.
in white paint, 236.
— — in coral mud, 490.
■ at Ascension, 521.
Insects, first colonists of St. Paul's
rocks, 20.
blown out to sea, 173.
of Patagonia, 184, 346.
of Tierra del Fuego, 254.
of Galapagos, 403, 415, 416.
of Keeling Island, 481.
of St. Helena, 516.
Instincts of birds, 107, 422.
Iodine with salt at Iquique, 385.
Iquique, 383.
Iron, oxide of, on rocks, 2^
Islands, oceanic, volcanic, 19.
, Antarctic, 264.
, floating, 282.
, low, 425, 492.
Jackson, Col., on frozen snow, 344.
Jaguar, habits of, 147.
Jajuel, mines of, 276.
James Island, Galapagos Archipel-
ago, 398.
Juan Fernandez, volcano of, 329.
, flora of, 416.
Rater's Peak, 227.
Kauri pine, 451.
Keeling Island, 477.
, birds of, 480.
, entomology of, 488.
, flora of, 479.
542
INDEX
Keeling Island, subsidence of, 500.
Kelp, or sea-weed, 255.
Kendall, Lieut., on a frozen body,
265.
Kingfishers, 12, 151.
King George's Sound, 474.
Labourers, condition of, in Chile,
283.
Lagoon-islands, 425, 478, 491.
Lagostomus, 136.
Lake, brackish, near Rio, 31.
■ , with floating islands, 282.
■ formed during earthquake, 392.
Lamarck on acquired blindness, 62.
Lampyris, 40.
Lancaster, Capt., on a sea-tree, 112.
Land-shells, 368, 515, 516.
Lazo, 54, 167, 204.
Leaves, fall of, 251.
— — , fossil, 473.
Leeks in New Zealand, imported,
452.
Lepus Magellanicus, 208.
Lesson, M., on the scissor-beak, 151.
, on rabbit of the Falklands,
208.
Lichen on loose sand, 384.
Lichtenstein on ostriches, 104.
Lightning storms, 72.
> tubes, 70.
Lima, 386, 389.
, elevation of a river near, 379.
Lime, changed by lava into crystal-
line rock, 16.
Limnaea in brackish water, 31.
Lion-ant, 466.
Lizard, no.
, marine species of, 408.
Lizards, transport of, 405.
Llama or Guanaco, habits of, 179.
Locusts, 348.
Longevity of species in Mollusca, 94.
Lorenzo, San, island of, 388.
Low archipelago, 425.
Lund, M., on antiquity of man,
379.
Lund and Clausen on fossils of
Brazil, 143, 187.
Luxan, 348.
Luxuriant vegetation not necessary
to support large animals, 97.
Lycosa, 46.
Lyell, Mr., on terraces of Coquimbo,
363.
■ , on longevity of Mollusca, 95.
, on subsidence in the Pacific,
494-
, on change in vegetation, 132.
, on fossil horses' teeth, 143.
, on distribution of animals, 346.
, on frozen snow, 344.
■ , on extinct mammals and ice-
period, 188.
, on flocks of butterflies, 172.
— , on stones twisted by earth-
quakes, 326.
Macculloch on infection, 459.
Macquarie river, 467.
Macrauchenia, 94, 186.
Macrocystis, 255.
Madrina, or godmother of a troop
of mules, 334.
Magdalen Channel, 257.
Magellan, Strait of, 247.
Malcolmson, Dr., on hail, 128.
Maldiva atolls, 492, 501, 504.
Maldonado, 50.
Mammalia, fossil, 93, 140, 143, 169,
186, 392.
Man, antiquity of, 378.
, fossil remains of, 392.
, body frozen, 266. ^
, fear of, an acquired instinct,
424.
-, extinction of races, 459, 472.
movements in,
Mares' flesh eaten by troops, 114.
killed for their hides, 168.
Mastodon, 139, 142.
Matter, granular,
112.
Mauritius, 509.
Maypu river, 335.
Megalonyx, 93, 143.
Megatherium, 93,
Mendoza, climate
95, 143.
of, 343.
350.
Mexico, elevation of, 143.
Miasmata, 386, 459.
Mice inhabit sterile places, 380.
, number of, in America, 60.
, how transported, 305, 400.
different on opposite sides of
Andes, 346.
of the Galapagos, 400.
of Ascension, 518.
Millepora, 489.
Mills for grinding ores, 283.
Mimosae, 36.
Mimus, 65, 418, 422.
Miners, condition of, 277, 282, 359,
366.
Mines, 276, 360, 365.
— I — , how discovered, 336.
Missionaries at New Zealand, 449.
Mitchell, Sir T., on valleys of Aus-
tralia, 462.
Mocking-bird, 65, 418, 422.
Molina omits description of certain
birds, 288.
Molothrus, habits of, 63.
Monkeys with prehensile tails, 38.
Monte Video, 51, 155.
Moresby, Capt., on a great crab, 489.
on coral-reefs, 505.
Mount Sarmiento, 249, 257.
Tarn, 250.
Mountains, elevation of, 330.
Movements in granular matter, 112.
Mud, chalk-like, 490.
disturbed by earthquake, 325.
Mules, 334.
Muniz, Sig., on niata cattle, 159.
Murray, Mr., on spiders, 175.
INDEX
543
Mylodon, 94, 143, 169.
Myopotamus Coypus, 305.
Negress with goitre, 333.
Negro, Rio, 74, 162.
lieutenant, 87.
New Caledonia, reef of, 494, 496,
502.
Zealand, 440.
Niata cattle, 159.
Noises from a hill, 382.
Noses, ceremony of pressing, 447.
Nothura, 56.
Notopod, crustacean, 175.
Nulliporae, incrustations like, 20.
protecting reefs, 524.
Octopus, habits of, 17.
Oily coating on sea, 27,
Olfersia, 20.
Opetiorhynchus, 306.
Opuntia, 278.
Darwinii, 179.
Galapageia, 396.
Orange-trees self-sown, 132.
Ores, gold, 283.
Ornithology of Galapagos, 401, 418.
Ornithorhynchus, 466.
Osorno, volcano of, 290, 292, 309.
Ostrich, habits of, 53, 101.
Ostriches' eggs, 125.
Otaheite, 426.
Otter, 305.
Ova in sea, 27,
Oven-bird, 107.
Owen, Capt., on a drought in Africa,
145.
, Professor, on the Capybara,
60.
— , Professor, on fossil quadru-
peds, 93-96, 143-
, Professor, on nostrils of the
Gallinazo, 199.
Owl of Pampas, 81, 138.
Oxyurus, 253, 307.
Oysters, gigantic, 185.
Paint, white, 236.
Pallas on Siberia, 78,
Palm-trees in La Plata, 57.
in Chile, 273.
, south limit of, 260.
Palms absent at Galapagos, 397.
Pampas, number of embedded re-
mains in, 168.
, S. limit of, 86.
, changes in, 132.
■ not quite level, 135, 139, 156.
, geology of, 141, 168.
-, view of, from the Andes, 347.
Papilio feronia, 43.
Parana, Rio, 138, 151, 160.
, islands in, 147.
Parish, Sir W., on the great drought,
146.
Park, Mungo, on eating salt, 123.
Parrots, 151, 259.
Partridges, 56.
Pas, fortresses of New Zealand, 442.
Passes in Cordillera, 353.
Pasture, altered from grazing of
cattle, 131.
Patagones, 75.
Patagonia, geology of, 184, 348.
, zoology of, 179, 184, 193.
Patagonian Indians, 245.
Peach-trees, self-sown, 133.
Peat, formation of, 304.
Pebbles perforated, 162, 285.
transported in roots of trees,
^ 487.
Pelagic animals in southern ocean,
175.
Pelacanoides Berardii, 308.
Penas, Gulf of, 263.
Penguin, habits of, 214.
Pepsis, habits of, 46.
Pernambuco, reef of, 524.
Pernety on hill of ruins, 213.
on tame birds, 423.
Peru, 383-393-
, dry valleys of, 379, 383.
Petrels, habits of, 307.
Peuquenes, pass of, 338.
Phonolite at F. Noronha, 21.
Phosphorescence of the sea, 176.
of a coralline, 217.
of land insects and sea ani-
mals, 40.
Phryniscus, 109.
Pine of New Zealand, 451.
Plains at foot of Andes in
279, 335.
almost horizontal near St
Chile,
Fe,
139-
Planariae, terrestrial species of, 37.
Plants of the Galapagos, 396, 414,
419.
of Keeling Island, 479.
of St. Helena, 513.
Plata, Rio, 49.
, thunderstorms of, 72.
Plover, long-legged, 126.
Polished rocks, Brazil, 22.
Polyborus chimango, 66.
Novae Zelandise, 68.
■ Brasiliensis, 66.
Ponsonby Sound, 236.
Porpoises, 49.
Port Desire, 178.
, river of, 119, 184.
St. Julian, 184.
Famine, 249.
Portillo pass, 339, 344.
Porto Praya, 1.
Potato, wild, 302.
Potrero, Seco, 370.
Prairies, vegetation of, 132.
Prevost, M., on cuckoos, 64.
Priestley, Dr., on lightning-tubes,
70.
Procellaria gigantea, habits of, 307.
Proctotretus. no.
Proteus, blindness of, 62.
544
INDEX
Protococcus nivalis, 342.
Pteroptochos, two species of, 287.
, species of, 296, 306.
Puente del Inca, 354, 377.
Puffinus cinereus, 307.
Puma, habits of, 148, 198, 286.
, flesh of, 129.
Puna, or short respiration, 341.
Punta Alta, Bahia Blanca, 93.
Gorda, 142, 378.
Pyrophorus luminosus, 41.
Quadrupeds, fossil, 93, 139, 142,
168, 186.
, large, do not require luxuriant
vegetation, 97.
-, large, weight of, 99.
Quartz of the Ventana, 121.
of Tapalguen, 129.
of Falkland Island, 211.
>uedius, 20.
►uillota, valley of, 271.
>uintero, 270.
Juiriquina Island, 321.
|uoy and Gaimard on stinging
corals, 489.
on coral reefs, 502.
Rabbit, wild, at the Falkland Isl-
ands, 207.
Rain at Coquimbo, 358, 368, 369.
at Rio, 39.
and earthquakes, 372.
in Peru, 385, 386.
in Chile, formerly more abun-
dant, 378.
Chile,
358.
in
effects on vegetation,
Rana mascariensis, 404.
Rat, only aboriginal animal of New
Zealand, 451.
Rats at Galapagos, 400.
at Ascension, 519.
at Keeling Island, 481.
Rattle-snake, species with allied
habit, 108.
Red snow, 342.
Reduvius, 349.
Reef at Pernambuco of sandstone,
524.
Reefs of coral, 491-508.
, Barrier, 494-501.
, Fringing, 497.
Reeks, Mr., analysis of salt, 77,
, analysis of bones, 169.
, analysis of salt and shells, 391.
Remains, human elevated, 392.
Remedies of the Gauchos, 140.
Rengger on the horse, 249.
Reptiles absent in Tierra del Fuego,
2S4 * ^ ,
at Galapagos, 404.
Respiration difficult in Andes, 341.
Retrospect, 527.
Revolutions at Buenos Ayres, 153.
Rhinoceroses live in desert coun-
tries, 98.
Rhinoceroses, frozen, 100, 266.
Rhynchops nigra, 149.
Richardson, Dr., on mice of North
America, 401.
, on frozen soil, 101, 265.
, on eating fat, 130.
, on geographical distribution,
144.
Rimsky atoll, 492.
Rio de Janeiro, 29.
Plata, 49.
Negro, 74, 161.
Colorado, 81.
S. Cruz, 191.
, Sauce, 119.
Salado, 130.
Rivers, power of, in wearing chan-
nels, 194, 332.
River-bed, arched, 340.
River-courses dry in America, 119.
Rocks burnished with ferruginous
matter, 23.
Rodents, number of, in America, 60,
193.
, fossil species of, 94.
Rosas, General, 82, 115, 153.
Ruins of Callao, 390.
of Indian buildings in Cordil-
lera, 377, 389.
S. Cruz, 191.
Salado, Rio, 130.
Salinas at the Galapagos Archipel-
ago, 399.
in Patagonia, 76, 184.
Saline efflorescences, 89.
Salt with vegetable food, 122.
, superficial crust of, 385.
, with elevated shells, 391.
Salt-lakes, 76, 184, 399.
Sand, hot from sun's rays, at Gala-
pagos Archipelago, 399.
, noise from friction of, 382.
Sand-dunes, 86.
Sandstone of New South Wales, 462,
, reef of, 524.
Sandwich Archipelago, no frogs at,
404.
Land, 265.
San Pedro, forests of, 298.
Santa Cruz, river of, 191.
Santiago, Chile, 279.
Sarmiento, Mount, 249, 257.
Sauce, Rio, 119.
Saurophagus sulphureus, 64.
Scarus eating corals,- 490.
Scelidotherium, 93.
Scenery of Andes, 337.
Scissor-tail, 151.
Scissor-beak, habits of, 151.
Scoresby, Mr., on effects of snow 011
rocks, 337.
Scorpions, cannibals, 179.
Scrope, Mr., on earthquakes, 373.
Scytalopus fuscus, 253, 307.
Sea, open, inhabitants of, 176.
, phosphorescence of, 176.
INDEX
545
Sea, distant noise of, 314.
Sea-pen, habits of, in, 217.
Sea-weed, growth of, 255.
Seals, number of, 302.
Seeds transported by sea, 415, 479.
Serpulae, protecting reef, 525.
Shark killed by Diodon, 24.
Shaw, Dr., on lion's flesh, 129.
Sheep, infected, 460.
lines on Mon
land, in great numbers,
ep, ;
Shelley, lines on Mont Blanc, 182
Shells, land, in
368.
, land, at St. Helena, 515.
, fossil, of Cordillera, 339.
- of Galapagos, 413.
, elevated, 95, 143, 184, 270,
364, 391.
, tropical forms of, far south,
259.
, decomposition of, with salt,
39i.
Shepherds' dogs, 163.
Shingle-bed of Patagonia, 86, 186.
Siberia compared with Patagonia,
78.
, zoology of, related to North
America, 144.
Siberian animals, how preserved in
ice, 266.
— , animals, food necessary during
their existence, 101.
Silicified trees, 351, 373.
Silurian formations at Falkland
Islands, 212.
Silurus, habits of, 149.
Skunks, 92.
Slavery, 30, 33, 34, 525.
bmelhng power of carrion-hawks,
198.
Smith, Dr. Andrew, on the support
of large quadrupeds, 97.
, on perforated pebbles, 162.
Snake, venomous, 108.
Snow, effects of, on rocks, 337.
, prismatic structure of, 344.
, red, 342.
Snow-line on Cordillera, 261, 342,
_ 344-
Society, state of, in La Plata, 51,
170.
, state of, in Australia, 468.
■ ■ Archipelago, 425.
- Archipelago, volcanic phenom-
ena at, 500, 506.
Soda, nitrate of, 383.
— — , sulphate of, 89.
Soil, frozen, 100, 265.
Spawn on surface of sea, 27.
Species, distribution of, 142, 384.
— ;—, extinction of, 188.
Spiders, habits of, 45-48.
, gossamer, 172.
killed by and killing wasps,
45-48.
on Keeling Island, 481.
on St. Paul's, 20.
Springs, hot, 280.
Stephenson, Mr., on growth of sea-
weed, 256.
Stinging animals, 489.
St. Helena, 512.
, introduction of spirits into,
St. Fe, 140.
St. Jago, C. Verds, 1.
, C. Verds, unhealthiness of,
387.
St. Maria, elevated, 326, 328.
St. Paul's rocks, 18.
Stones perforated, 162, 285.
transported in roots, 487.
Storm, 232, 298.
in Cordillera, 342, 381.
Streams of stones at Falkland Islands,
211.
Strongylus, 43.
Struthio Rhea, 53, 105.
Darwinii, 105.
Strzelecki, Count, 472.
Suadiva atoll, 492.
Subsidence of coral reef, 492-508.
of Keeling Island, 500.
of Patagonia, 186.
of coast of Peru, 390.
of Cordillera, 340, 352.
■ of coasts of Chile, 365.
• of Vanikoro, 501.
of coral reefs great in amount,
504-
— , cause of distinctness in Ter-
tiary epochs, 366.
Sulphate of lime, 77 , 184, 390.
of soda incrusting the ground,
89.
of soda with common salt, 77,
on cuckoos, 63.
39i-
Swainson, Mr.
Sydney, 455.
Tabanus, 185.
Tahiti (Otaheite), 425.
, three zones of fertility, 429.
Talcahuano, 321.
Tambillos, Ruinas de, 377.
Tameness of birds, 422.
Tapacolo and Turco, 287.
Tapalguen, Sierra, flat hills of
quartz, 129.
Tarn, Mount, 250.
Tasmania, 471.
Tattooing, 427, 450.
Temperance of the Tahitians, 435.
Temperature of Tierra del Fuego
and Falkland Islands, 258.
of Galapagos, 395, 399.
Tercero, Rio, fossils in banks of, 139.
Terraces in valleys of Cordillera,
334-
of Coquimbo, 363.
of Pf.tagonia, 185, 195.
Tertiary formations of the Pampas,
93, 142, 168.
formations of Patagonia, 184,
348.
VOL. XXIX— R
HC
546
INDEX
Tertiary formations in Chile, epochs
of, 365.
Teru-tero, habits of, 127.
Testudo, habits of, 405, 417.
Theory of lagoon-islands, 497.
Theristicus, 179.
Thistle beds, 131, 136, 161.
Thunder-storms, 72.
Tierra del Fuego, 219-268.
, climate and vegetation of, 258.
, zoology of, 252.
, entomology of, 254.
Tinamus rufescens, 125.
Tinochorus Eschscholtzii, 106.
Toad, habits of, 109.
not found in oceanic islands,
404.
Torrents in Cordillera, 335, 340.
Tortoise, habits of, 405, 417.
Toxodon, 94, 139, 142, 168.
Transparency of air in Andes, 345.
of air in St. Jago, 14.
Transport of seeds, 415, 479.
■ of boulders, 201, 264.
of stones in, roots of trees, 487.
of fragments of rock on banks
of the St. Cruz river, 194.
Travertin with leaves of trees, Van
Diemen's Land, 473.
Tree-ferns, southern limits of, 261.
, 473-
Trees, absence of, in Pampas, 56.
— ■ — , floating, transport stones, 487.
, silicified, vertical, 351.
, silicified, size of, 373.
, time required to rot, 320.
Tres Montes, 299.
Trichodesmium, 25.
Trigonocephalus, 108.
Tristan d'Acunha, 424, 481.
Trochilus, 289.
Tropical scenery, 521.
Tschudi, M., on subsidence, 390.
Tubes, silicious, formed by light-
ning, 70.
Tucutuco, habits of, 61.
, fossil species of, 94.
Tuff, craters of, 395.
, Infusoria in, 521.
Tupungato, volcano of, 344.
Turco, El, 287.
Turkey buzzard, 69, 199, 302.
Turtle, manner of catching, 484.
Type of organization in Galapagos
Islands, American^ 416.
Types of organization in different
countries, constant, 188.
Tyrannus, 151.
Ulloa on hydrophobia, 374.
on Indian buildings, 378.
Unanue, Dr., on hydrophobia, 374.
Uruguay, Rio, 152, 160.
, not crossed by the Bizcacha,
136.
Uspallata range and pass, 351.
Vacas, Rio, 353.
Valdivia, 315.
, forests of, 316, 32a
Valley of St. Cruz, how excavated,
195.
, dry, at Copiapo, 376.
Valleys, excavation of, in Chile,
334, 37§
Tahiti, 431, 435.
in Cordillera, 334.
of New South Wales, 462.
Valparaiso, 269, 332.
Vampire bat, 32.
Vapour from forests, 34.
Van Diemen's Land, 470%
Vanellus Cayanus, 127.
Vanessa, flocks of, 172.
Vanikoro, 495, 496, 501.
Vegetation of St. Helena, changes
of, 515.
Vegetation on opposite sides of Cor-
dillera, 346.
, luxuriant, not necessary to
support large animals, 97.
Ventana, Sierra, 122.
Verbena melindres, 51.
Villa Vicencio, 351.
Virgularia Patagonica, III, 217.
Volcanic bombs, 520.
Islands, 18.
■ phenomena, 329.
Volcanoes near Chiloe, 290, 292,
309, 329. _ , . ..
, their presence determined by
elevation or subsidence, 506.
Vultur aura, 69, 199, 301.
Waders, first colonists of distant
islands, 402.
Waimate, New Zealand, 445.
Walckenaer, on spiders, 48.
Walleechu tree, 79.
Wasps preying on spiders and killed
by, 46-48.
Water, sold at Iquique, 383.
, fresh, floating on salt, 49, 483.
Water-hog, 60.
Waterhouse, Mr., on Rodents, 60,
400.
, on the Niata ox, 159.
, on the insects of Tierra del
Fuego, 254. ■
-, on the insects of Galapagos,
404, 415.
Waves, caused by fall of ice, 240,
262.
from earthquakes, 324, 327.
Weather, connection with earth-
quakes, 372.
Weather-board, N. S. Wales, 461.
Weeds in New Zealand, imported,
415, 452.
Weight of large quadrupeds, 99.
Wellington, Mount, 473.
Wells, ebbing and flowing, 483.
at Iquique, 384.
West Indies, banks of, 463.
1 coral reefs of, 498, 506.
INDEX
547
West Indies, zoology of, 144.
Whales, oil from, 27.
leaping out of water, 239.
White, Mr., on Spiders, 46.
Wigwams of Fuegians ; 227.
Williams, Rev., on infectious dis-
orders, 459. #
Winds, dry, in Tierra del Fuego,
247.
at the Cape Verds, 13.
, cold, in Cordillera, 381.
on Cordillera, 342.
Winter's Bark, 251, 298.
Wolf at the Falklands, 208.
Wood, Capt., on the Agouti, 81.
Woollya, 237.
Yaquil, 282.
Yeso, Valle del, 338.
York Minster, 223.
Zonotrichia, 63.
Zoological provinces of N. and S.
America. 144.
Zoology or Galapagos, 400.
of Keeling Island, 480.
of Tierra del Fuego, 252.
of Chonos Islands, 305.
of St. Helena, 516.
Zoophytes, 112.
at Falkland Islands, ai5.
Zorillo, or skunk, 92.
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