Himalayan Journals — Volume 2: Or, Notes of a Naturalist in Bengal, the Sikkim and Nepal Himalayas, the Khasia Mountains, etc.Hooker, Joseph Dalton
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Himalayan Journals — Volume 2: Or, Notes of a Naturalist in Bengal, the Sikkim and Nepal Himalayas, the Khasia Mountains, etc.
Hooker, Joseph Dalton
Himalaya Mountains -- Description and travel; Natural history -- Himalaya Mountains
The most prominent effect of the steepness of the valleys is the
prevalence of land-slips, which sometimes descend for 3000 feet,
carrying devastation along their course: they are caused either by
the melting of the snow-beds on the mountains, or by the action of
the rains on the stratified rocks, and are much increased in effect
and violence by the heavy timber-trees which, swaying forwards,
loosen the earth at their roots, and give impetus to the mass.
This phenomenon is as frequent and destructive as in Switzerland,
where, however, more lives are lost; from the country being more
populous, and from the people recklessly building in places
particularly exposed to such accidents. A most destructive one had,
however, occurred here the previous year, by which a village was
destroyed, together with twelve of its inhabitants, and all the
cattle. The fragments of rock precipitated are sometimes of enormous
size, but being a soft mica-schist, are soon removed by weathering.
It is in the rainy season that landslips are most frequent, and
shortly after rain they are pretty sure to be heard far or near.
I crossed the debris of the great one alluded to, on the first march
beyond Singtam: the whole face of the mountain appeared more or less
torn up for fully a mile, presenting a confused mass of white
micaceous clay, full of angular masses of rock. The path was very
difficult and dangerous, being carried along the steep slope, at an
angle, in some places, of 35 degrees; and it was constantly shifting,
from the continued downward sliding, and from the action of streams,
some of which are large, and cut deep channels. In one I had the
misfortune to lose my only sheep, which was carried away by the
torrent. These streams were crossed by means of sticks and ricketty
bamboos, and the steep sides (sometimes twenty or thirty feet high),
were ascended by notched poles.
The weather continued very hot for the elevation (4000 to 5000 feet),
the rain brought no coolness, and for the greater part of the three
marches between Singtam and Chakoong, we were either wading through
deep mud, or climbing over rocks. Leeches swarmed in incredible
profusion in the streams and damp grass, and among the bushes: they
got into my hair, hung on my eyelids, and crawled up my legs and down
my back. I repeatedly took upwards of a hundred from my legs, where
the small ones used to collect in clusters on the instep: the sores
which they produced were not healed for five months afterwards, and I
retain the scars to the present day. Snuff and tobacco leaves are the
best antidote, but when marching in the rain, it is impossible to
apply this simple remedy to any advantage. The best plan I found to
be rolling the leaves over the feet, inside the stockings, and
powdering the legs with snuf.
Public-domain text, read in full here on John Shaqi.
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