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
On the 29th of August I left Lachoong and proceeded up the valley.
The road ran along a terrace, covered with long grass, and bounded by
lofty banks of unstratified gravel and sand, and passed through
beautiful groves of green pines, rich in plants. No oak nor chesnut
ascends above 9000 feet here or elsewhere in the interior of Sikkim,
where they are replaced by a species of hazel (_Corylus_); in the
North Himalaya, on the other hand, an oak (_Quercus semecarpifolia,_
see vol. i., chapter viii) is amongst the most alpine trees, and the
nut is a different species, more resembling the European. On the
outer Sikkim ranges oaks (_Q. annulata?_) ascend to 10,000 feet, and
there is no hazel. Above the fork, the valley contracts extremely,
and its bed is covered with moraines and landslips, which often bury
the larches and pines. Marshes occur here and there, full of the
sweet-scented Hierochloe grass, the Scotch _Thalictrum alpinum,_ and
an _Eriocaulon,_ which ascends to 10,000 feet. The old moraines were
very difficult to cross, and on one I found a barricade, which had
been erected to deceive me regarding the frontier, had I chosen this
route instead of the Lachen one, in May.
Broad flats clothed with rhododendron, alternate with others covered
with mud, boulders, and gravel, which had flowed down from the gorges
on the west, and which still contained trees, inclined in all
directions, and buried up to their branches; some of these debacles
were 400 yards across, and sloped at an angle of 2 degrees to 3
degrees, bearing on their surfaces blocks fifteen yards in diameter.*
[None were to be compared in size and extent with that at Bex, at the
mouth of the Rhone valley.] They seem to subside materially, as I
perceived they had left marks many feet higher on the tree-trunks.
Such debacles must often bury standing forests in a very favourable
material, climate, and position for becoming fossilized.
Public-domain text, read in full here on John Shaqi.
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