A naturalist in Madagascar: A record of observation, experiences, and impressions made during a period of over fifty years' intimate association with the natives and study of the animal & vegetable life of the islandSibree, James
History
A naturalist in Madagascar: A record of observation, experiences, and impressions made during a period of over fifty years' intimate association with the natives and study of the animal & vegetable life of the island
Sibree, James
Madagascar; Natural history -- Madagascar
On Saturday morning we came to the bank of the Ikòpa, which river
is at some points half-a-mile or more wide, but then at its lowest
level, being apparently very shallow, but so interrupted everywhere
with shelves of rock that it would be difficult for even a small
canoe to make its way far. There were numerous islands, covered with
bamboo, bàraràta, _rofìa_-palms and other vegetation. From a low hill
we had a view over an immense expanse of flat country on the western
side of the river. Only here and there was the level broken by a
line of hills of small elevation. After leaving the Ikòpa we found
ourselves in a very different kind of country from any we had yet
passed through, a succession of low hills or mamelons of dry sandy
gravel, with hardly any vegetation, and looking as if no rain had
fallen upon it for years. In the afternoon I noticed that a large
number of granite boulders were strewn over the country, and could
hardly doubt that these, from their rounded forms, but especially
from the absence, as far as I could see, of any such rock _in situ_,
must by some means or other have been transported from the granitic
region of the interior far to the eastward. Must this not have been
glacier or iceberg action? Although it is difficult to understand
such agency in the tropics.
Ten years after making the journey, my friend, Mr Baron, in
travelling across the island towards the north-west coast, but about
a hundred and twenty miles farther north, came across isolated
rocks, which were quite different in composition from anything near
them. Of these he said: “I could think of no agent to account for
their occurrence but that of glacial action. They seemed to me to be
perched blocks, as there was no hill near from which they could have
fallen, nor any rock of the kind _in situ_.” I was interested to find
that an expert in Madagascar geology like Mr Baron had come to the
same conclusion as myself with regard to these granite boulders.
Early in the afternoon we arrived at Mèvatanàna, the most important
place in this part of the country, with about a hundred houses; it
had, however, been quite recently burnt down, but was in process of
rebuilding. The houses seemed rather larger than those in Imèrina,
made of round-pole framework, filled in with _bàraràta_ stems, the
roofs of _rofìa_-palm leaf-stalks and thatched with grass. We secured
a new house, not quite finished; and as this was very like a large
birdcage, besides having no doors in the three doorways, we put up
the tent on one side, piled up our heavy luggage against another of
the doorways, and hung a rug over the third, so as to make ourselves
less of a public spectacle.
Public-domain text, read in full here on John Shaqi.
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