Travels in the Central Parts of Indo-China (Siam), Cambodia, and Laos (Vol. 1 of 2): During the Years 1858, 1859, and 1860Mouhot, Henri
History
Travels in the Central Parts of Indo-China (Siam), Cambodia, and Laos (Vol. 1 of 2): During the Years 1858, 1859, and 1860
Mouhot, Henri
Cambodia -- Description and travel; Khmer language; Natural history -- Indochina; Thailand -- Description and travel
I bought, for twenty-five ticals, a small boat to enable me to visit
the isles of the gulf. The first I landed at was named Konam-sao; it
is in the form of a cone, and nearly 250 metres[11] in height, but
only two miles in circumference. Like all the other islands in this
part of the gulf, it is of volcanic origin. The rocks which surround
it make the access difficult; but the effect produced by the richness
and bright green of the vegetation is charming. The dry season, so
agreeable for European travelling, from the freshness of the nights and
mornings, is in Siam a time of stagnation and death for all nature;
the birds fly to the neighbourhood of houses, or to the banks of the
rivers, which furnish them with nourishment; rarely does their song
come to enchant the listener; and the fishing-eagle alone utters
his hoarse and piercing cry every time the wind changes. Ants swarm
everywhere, and appear to be, with the mosquitoes and crickets, the
only insects that have escaped destruction.
[11] A metre is equivalent to 3 feet 3⅓ inches.
Nowhere did I find in these islands the slightest trace of path or
stream; and it was extremely difficult to advance at all through the
masses of wild vine and interwoven branches. I was forced to make my
way, hatchet in hand, and returned at night exhausted with the heat and
fatigue.
The greater portion of the rocks in the elevated parts of these islands
is elementary, and preserves traces of their ancient deposit beneath
the waters. They have, however, undergone considerable volcanic
changes, and contain a number of veins and irregular deposits of the
class known as contact deposits that are formed near the junction of
stratified rocks with intruded igneous masses.
KO-MAN ISLANDS.
On the 26th we set sail for the first of the Ko-Man islands, for there
are three, situated close together, bearing this name. The largest is
only twelve miles from the coast. Some fishing-eagles, a few black
doves, and a kind of white pigeon were the only winged creatures I
saw. Iguanas are numerous, and when in the evening they come out of
their retreats, they make such a noise in walking heavily over the dead
leaves and branches, that one might suppose it caused by animals of a
much larger size.
Toward evening, the tide having fallen, I allowed my boat to ground
on the mud, which I had remarked during the day to be like a peat-bog
impregnated with volcanic matter; and during the whole night so strong
a sulphureous odour escaped from it, that I imagined myself to be over
a submarine volcano.
On the 28th we passed on to the second island, which is higher and
more picturesque than the other. The rocks which surround it give it
a magnificent effect, especially in a bright sunlight, when the tide
is low. The isles of the Patates owe their name to the numerous wild
tubers found there.
[Illustration:
Drawn by M. Sabatier, from a Sketch by M. Mouhot.
VIEW OF PAKNAM ON THE MENAM.]
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