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
The view of the Kinchin range from this spot being one of the finest in
Sikkim, and the place itself being visible from Dorjiling, I took a
very careful series of bearings, which, with those obtained at
Pemiongchi, were of the utmost use in improving my map, which was
gradually progressing. To my disappointment I found that neither priest
nor people knew the name of a single snowy mountain. I also asked in
vain for some interpretation of the lines I have quoted at page 365;
they said they were Lepcha worship, and that they only used them for
the gratification of the people, on the day of the great festival of
Kinchinjunga.
Hence I descended to the Kulhait river, on my route back to Dorjiling,
visiting my very hospitable tippling friend, the Kajee of Lingcham, on
the way down: he humbly begged me to get him a pair of spectacles, for
no other object than to look wise, as he had the eyes of a hawk; he
told me that mine drew down universal respect in Sikkim, and that I had
been drawn with them on, in the temple at Changachelling; and that a
pair would not only wonderfully become him, but afford him the most
pleasing recollections of myself. Happily I had the means of gratifying
him, and have since been told that he wears them on state occasions.
I encamped by the river, 3,160 feet above the sea, amongst figs and
plantains, on a broad terrace of pebbles, boulders and sand, ten feet
above the stream; the rocks in the latter were covered with a red
conferva. The sand on the banks was disposed in layers, alternately
white and red, the white being quartz, and the red pulverised garnets.
The arranging of these sand-bands by the water must be due to the
different specific gravities of the garnet and quartz; the former being
lighter, is lifted by the current on to the surface of the quartz, and
left there when the waters retire.
On the next day I ascended Hee hill, crossed it at an elevation of
7,290 feet, and camped on the opposite side at 6,680 feet, in a dense
forest. The next march was still southward to the little Rungeet
guard-house, below Dorjiling spur, which I reached after a fatiguing
walk amidst torrents of rain. The banks of the little Rungeet river,
which is only 1,670 feet above the sea, are very flat and low, with
broad terraces of pebbles and shingle, upon which are huge gneiss
boulders, fully 200 feet above the stream.
Public-domain text, read in full here on John Shaqi.
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