Himalayan Journals — Complete: 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 — Complete: 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
[109] At sunrise the temperature was 11·5°; that of grass, cleared on
the previous day from snow, and exposed to the sky, 6·5°; that on
wool, 2·2°; and that on the surface of the snow, 0·7°.
Before sunrise the atmosphere was still, and all but cloudless. To the
south-east were visible the plains of India, at least 140 miles
distant; where, as usual, horizontal layers of leaden purple vapour
obscured the horizon: behind these the sun rose majestically, instantly
dispersing them, while a thin haze spread over all the intervening
mountains, from its slanting beams reaching me through otherwise
imperceptible vapours: these, as the sun mounted higher, again became
invisible, though still giving that transparency to the atmosphere and
brilliant definition of the distances, so characteristic of a damp, yet
clear day.
Mon Lepcha commands a most extensive view of Sikkim, southward to
Dorjiling. At my feet lay the great and profound valley of the Ratong,
a dark gulf of vegetation. Looking northward, the eye followed that
river to the summit of Kinchinjunga (distant eighteen miles), which
fronts the beholder as Mont Blanc does when seen from the mountains on
the opposite side of the valley of Chamouni. To the east are the
immense precipices and glaciers of Pundim, and on the west those of
Kubra, forming great supporters to the stupendous mountain between
them. Mon Lepcha itself is a spur running south-east from the Kubra
shoulder: it is very open, and covered with rounded hills for several
miles further north, terminating in a conspicuous conical black
hummock[110] called Gubroo, of 15,000 feet elevation, which presents a
black cliff to the south.
[110] This I have beau told is the true Kubra; and the great snowy
mountain behind it, which I here, in conformity with the Dorjiling
nomenclature, call Kubra, has no name, being considered a part of
Kinchin.
Kinchinjunga rises in three heads, of nearly equal height,[111] which
form a line running north-west. It exposes many white or grey rocks,
bare of snow, and disposed in strata[112] sloping to the west; the
colour of all which above 20,000 feet, and the rounded knobbed form of
the summit, suggest a granitic formation. Lofty snowed ridges project
from Kubra into the Ratong valley, presenting black precipices of
stratified rocks to the southward. Pundim has a very grand appearance;
being eight miles distant, and nearly 9000 feet above Mon Lepcha, it
subtends an angle of 12°; while Kinchin top, though 15,000 feet higher
than Mon Lepcha, being eighteen miles distant, rises only 9° 30 minutes
above the true horizon: these angular heights are too small to give
much grandeur and apparent elevation to mountains, however lofty; nor
would they do so in this case, were it not that the Ratong valley which
intervenes, is seen to be several thousand feet lower, and many degrees
below the real horizon.
[111] The eastern and western tops, are respectively 27,826 and 28,177
feet above the level of the sea.
Public-domain text, read in full here on John Shaqi.
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