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
It may just be said further, that the slopes of the crater both
inside and out are covered with turf, which grows on a dark brown
volcanic soil, mingled with rounded pebbles of greenish or purple
lava, very compact and close in structure, and containing minute
crystals scattered sparingly through it. Occasional blocks of this
are found round the edge of the crater wall, and the same rock crops
out at many places on the steep inner slopes. I did not notice any
vesicular lava or scoria; and at a little homestead not far from the
north-eastern foot of Trìtrìva, I was surprised to find the _hàdy_
or fosse dug to twelve or fourteen feet deep almost entirely through
the red clay or earth found all through the central regions of the
island. The dark brown volcanic soil, here seen in section, appeared
to be only eighteen inches deep, with layers of small pebbles. So
that the discharge of the volcanic dust and ash appears to have
extended only a short distance from the mountain; at least it does
not appear to have been very deep, unless, indeed, there has been
much denudation. It must be remembered, however, that this point
is to the windward side of the hill; probably the volcanic soil is
deeper to the west of it. The much greater height of the western
wall of the crater is no doubt due to the prevailing easterly winds
carrying the bulk of the ejected matter to the west, and piling it up
to two or three times the height of the eastern side. After seeing
the amount of gneiss rock which must have been blown out of the
vent, I expected to have found much greater quantities of it, and in
larger blocks, than the very few and small fragments actually seen on
the outer slopes. The greater portion, however, is probably covered
up under the quantities of volcanic dust and _lapilli_ which were
subsequently ejected.
Trìtrìva, it will be evident from this slight sketch, will greatly
interest those who have a taste for geology and physical geography;
while its peculiar and somewhat awe-striking beauty makes it equally
worthy of a visit from the artist and the lover of the picturesque.
Certainly it became photographed upon our memory with a distinctness
which rendered it a vivid mental picture for many a day afterwards.
[Sidenote: VOLCANO OF ANKÀRATRA]
Public-domain text, read in full here on John Shaqi.
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