Himalayan Journals — Volume 1: Or, Notes of a Naturalist in Bengal, the Sikkim and Nepal Himalayas, the Khasia Mountains, etc.Hooker, Joseph Dalton
History
Himalayan Journals — Volume 1: 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 old and new Mechi rivers are several miles apart, but flow in the
same depression, a low swamp many miles broad, which is grazed at
this season, and cultivated during the rains. The grass is very rich,
partly owing to the moisture of the climate, and partly to the
retiring waters of the rivers; both circumstances being the effects
of proximity to the Himalaya. Hence cattle (buffalos and the common
humped cow of India) are driven from the banks of the Ganges 300
miles to these feeding grounds, for the use of which a trifling tax
is levied on each animal. The cattle are very carelessly herded, and
many are carried off by tigers.
Having returned to Titalya, Mr. Hodgson and I set off in an eastern
direction for the Teesta river, whose embouchure from the mountains
to the plains I was anxious to visit. Though the weather is hot, and
oppressively so in the middle of the day, there are few climates more
delicious than that of these grassy savannahs from December to March.
We always started soon after daybreak on ponies, and enjoyed a twelve
to sixteen miles' gallop in the cool of the morning before breakfast,
which we found prepared on our arrival at a tent sent on ahead the
night before. The road led across an open country, or followed paths
through interminable rice-fields, now dry and dusty. On poor soil a
white-flowered _Leucas_ monopolized the space, like our charlock and
poppy: it was apparently a pest to the agriculturist, covering the
surface in some places like a sprinkling of snow. Sometimes the
river-beds exposed fourteen feet of pure stratified sand, with only
an inch of vegetable soil above.
At this season the mornings are very hazy, with the thermometer at
sunrise 60 degrees; one laid on grass during the night falling 7
degrees below that temperature: dew forms, but never copiously: by
10 a.m. the temperature has risen to 75 degrees, and the faint
easterly morning breezes die away; the haze thickens, and covers the
sky with a white veil, the thermometer rising to 82 degrees at noon,
and the west wind succeeding in parching tornados and furious gusts,
increasing with the temperature, which attains its maximum in the
afternoon, and falling again with its decline at sunset. The evenings
are calm; but the earth is so heated, that the thermometer stands at
10 p.m. at 66 degrees, and the minimum at night is not below 55
degrees: great drought accompanies the heat at this season, but not
to such a degree as in North-west India, or other parts of this
meridian further removed from the hills. In the month of March, and
during the prevalence of west winds, the mean temperature was 79
degrees, and the dew-point 22 degrees lower, indicating great
drought. The temperature at Calcutta was 7 degrees warmer, and the
atmosphere very much damper.
Public-domain text, read in full here on John Shaqi.
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