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
Before proceeding to the pass, I turned off to the east, and
re-ascended Donkia to upwards of 19,000 feet, vainly hoping to get a
more distant view, and other bearings of the Tibetan mountains.
The ascent was over enormous piles of loose rocks split by the frost,
and was extremely fatiguing. I reached a peak overhanging a steep
precipice, at whose base were small lakes and glaciers, from which
flowed several sources of the Lachen, afterwards swelled by the great
affluent from Cholamoo lake. A few rocks striking north-east and
dipping north-west, projected at the very summit, with frozen snow
amongst them, beyond which the ice and precipices rendered it
impossible to proceed: but though exposed to the north, there was no
perpetual snow in the ordinary acceptation of the term, and an arctic
European lichen (_Lecidea oreina_) grew on the top, so faintly
discolouring the rocks as hardly to be detected without a
magnifying-glass.
I descended obliquely, down a very steep slope of 35 degrees, over
upwards of a thousand feet of debris, the blocks on which were so
loosely poised on one another, that it was necessary to proceed with
the utmost circumspection, for I was alone, and a false step would
almost certainly have been followed by breaking a leg. The alternate
freezing and thawing of rain amongst these masses, must produce a
constant downward motion in the whole pile of debris (which was
upwards of 2000 feet high), and may account for the otherwise
unexplained phenomenon of continuous shoots of angular rocks reposing
on very gentle slopes in other places.* [May not the origin of the
streams of quartz blocks that fill gently sloping broad valleys
several miles long, in the Falkland Islands, be thus explained? (See
"Darwin's Journal," in Murray's Home and Col. Lib.) The extraordinary
shifting in the position of my thermometer left among the rocks of
the Donkia pass (see chapter xxii), and the mobile state of the
slopes I descended on this occasion, first suggested this explanation
to me. When in the Falkland Islands I was wholly unable to offer any
explanation of the phenomenon there, to which my attention had been
drawn by Mr. Darwin's narrative.]
Public-domain text, read in full here on John Shaqi.
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