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 view from the summit commands the whole castellated front of
Kinchinjhow, the sweep of the Donkia cliffs to the east,
Chango-khang's blunt cone of ribbed snow* [This ridging or furrowing
of steep snow-beds is explained at vol. i, chapter x.] over head,
while to the west, across the grassy Palung dunes rise Chomiomo, the
Thlonok mountains, and Kinchinjunga in the distance.* [The latter
bore 241 degrees 30 minutes; it was distant about thirty-four miles,
and subtended an angle of 3 degrees 2 minutes 30 seconds. The rocks
on its north flanks were all black, while those forming the upper
10,000 feet of the south face were white: hence, the top is probably
granite, overlaid by the gneiss on the north.] The Palung plains, now
yellow with withered grass, were the most curious part of the view:
hemmed in by this range which rises 2000 feet above them, and by the
Lachen hills on the east, they appeared a dead level, from which
Kinchinjhow reared its head, like an island from the ocean.* [It is
impossible to contemplate the abrupt flanks of all these lofty
mountains, without contrasting them with the sloping outlines that
prevail in the southern parts of Sikkim. All such precipices are, I
have no doubt, the results of sea action; and all posterior influence
of sub-aerial action, aqueous or glacial, tends to wear these
precipices into slopes, to fill up valleys and to level mountains. Of
all such influences heavy rain-falls and a luxuriant vegetation are
probably the most active; and these features are characteristic of
the lower valleys of Sikkim, which are consequently exposed to very
different conditions of wear and tear from those which prevail on
these loftier rearward ranges.] The black tents of the Tibetans were
still there, but the flocks were gone. The broad fosse-like valley of
the Chachoo was at my feet, with the river winding along its bottom,
and its flanks dotted with black juniper bushes.
The temperature at this elevation, between 1 and 3 p.m., varied from
38 degrees to 59 degrees; the mean being 46.5 degrees, with the
dew-point 34.6 degrees. The height I made 17,585 feet by barometer,
and 17,517 by boiling-point. I tried the pulses of eight, persons
after two hours' rest; they varied from 80 to 112, my own being 104.
As usual at these heights, all the party were suffering from
giddiness and headaches.
Public-domain text, read in full here on John Shaqi.
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