Himalayan Journals — Volume 2: Or, Notes of a Naturalist in Bengal, the Sikkim and Nepal Himalayas, the Khasia Mountains, etc.Hooker, Joseph Dalton
History
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
Camp on Zemu river -- Scenery -- Falling rocks -- Tukcham mountain --
Height of glaciers -- Botany -- Gigantic rhubarb -- Insects -- Storm
-- Temperature of rivers -- Behaviour of Lachen Phipun -- Hostile
conduct of Bhoteeas -- View from mountains above camp -- Descend to
Zemu Samdong -- Vegetation -- Letters from Dorjiling -- Arrival of
Singtam Soubah -- Presents from Rajah -- Parties collecting
Arum-roots -- Insects -- Ascend Lachen river -- Thakya-zong -- Tallum
Samdong village -- Cottages -- Mountains -- Plants -- Entomology --
Weather -- Halo -- Diseases -- Conduct of Singtam Soubah -- His
character and illness -- Agrees to take me to Kongra Lama -- Tungu --
Appearance of country -- Houses -- Poisoning by arum-roots -- Yaks
and calves -- Tibet ponies -- Journey to Kongra Lama -- Tibetan tents
-- Butter, curds, and churns -- Hospitality -- Kinchinjhow and
Chomiomo -- Magnificent Scenery -- Reach Kongra Lama Pass.
My little tent was pitched in a commanding situation, on a rock fifty
feet above the Zemu, overlooking the course of that river to its
junction with the Thlonok. The descent of the Zenlu in one thousand
feet is more precipitous than that of any other river of its size
with which I am acquainted in Sikkim, yet immediately above my camp
it was more tranquil than at any part of its course onwards to the
plains of India, whether as the Zemu, Lachen or Teesta. On the west
bank a fine mountain rose in steep ridges and shrubby banks to 15,000
feet; on the east a rugged cliff towered above the stream, and from
this, huge masses of rock were ever and anon precipitated into the
torrent, with a roar that repeatedly spread consternation amongst us.
During rains especially, and at night, when the chilled atmospheric
currents of air descend, and the sound is not dissipated as in the
day-time, the noise of these falls is sufficiently alarming. My tent
was pitched near the base of the cliff, and so high above the river,
that I had thought it beyond the reach of danger; but one morning I
found that a large fragment of granite had been hurled during the
night to my very door, my dog having had a very narrow escape.
To what depth the accumulation at the base of this cliff may reach, I
had no means of judging, but the rapid slope of the river-bed is
mainly due to this, and to old moraines at the mouth of the valley
below. I have seen few finer sights than the fall of these stupendous
blocks into the furious torrent, along which they are carried amid
feathery foam for many yards before settling to rest.
Across the Thlonok to the southwards, rose the magnificent mountain
of Tukcham, but I only once caught a glimpse of its summit, which
even then clouded over before I could get my instruments adjusted for
ascertaining its height. Its top is a sharp cone, surrounded by rocky
shoulders, that rise from a mass of snow. Its eastern slope of 8000
feet is very rapid (about 38 degrees) from its base at the Zemu river
to its summit.
Public-domain text, read in full here on John Shaqi.
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