Himalayan Journals — Volume 1: Or, Notes of a Naturalist in Bengal, the Sikkim and Nepal Himalayas, the Khasia Mountains, etc.Hooker, Joseph Dalton
History
Himalayan Journals — Volume 1: 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
In the contracted parts of the valley, the mountains often dip to the
river-bed, in precipices of gneiss, under the ledges of which wild
bees build pendulous nests, looking like huge bats suspended by their
wings; they are two or three feet long, and as broad at the top,
whence they taper downwards: the honey is much sought for, except in
spring, when it is said to be poisoned by Rhododendron flowers, just
as that, eaten by the soldiers in the retreat of the Ten Thousand,
was by the flowers of the _R. ponticum._
Above these gorges are enormous accumulations of rocks, especially at
the confluence of lateral valleys, where they rest upon little flats,
like the river-terraces of Mywa, but wholly formed of angular
shingle, flanked with beds of river-formed gravel: some of these
boulders were thirty or forty yards across, and split as if they had
fallen from a height; the path passing between the fragments.* [The
split fragments I was wholly unable to account for, till my attention
was directed by Mr. Darwin to the observations of Charpentier and
Agassiz, who refer similar ones met with in the Alps, to rocks which
have fallen through crevasses in glaciers.--See "Darwin on Glaciers
and Transported Boulders in North Wales." London, "Phil. Mag." xxi.
p. 180.] At first I imagined that they had been precipitated from the
mountains around; and I referred the shingle to land-shoots, which
during the rains descend several thousand feet in devastating
avalanches, damming up the rivers, and destroying houses, cattle, and
cultivation; but though I still refer the materials of many such
terraces to this cause, I consider those at the mouths of valleys to
be due to ancient glacial action, especially when laden with such
enormous blocks as are probably ice-transported.
A change in the population accompanies that in the natural features
of the country, Tibetans replacing the Limboos and Khass-tribes of
Nepal, who inhabit the lower region. We daily passed parties of ten
or a dozen Tibetans, on their way to Mywa Guola, laden with salt;
several families of these wild, black, and uncouth-looking people
generally travelling together. The men are middle-sized, often tall,
very square-built and muscular; they have no beard, moustache, or
whiskers, the few hairs on their faces being carefully removed with
tweezers. They are dressed in loose blanket robes, girt about the
waist with a leather belt, in which they place their iron or brass
pipes, and from which they suspend their long knives, chopsticks,
tobacco-pouch, tweezers, tinder-box, etc. The robe, boots, and cap
are grey, or striped with bright colours, and they wear skull-caps,
and the hair plaited into a pig-tail.
Public-domain text, read in full here on John Shaqi.
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