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
The country continued a grassy level, with marshes and rice
cultivation, to the first range of hills, beyond which the river is
unnavigable; there also a forest commences, of oaks, figs, and the
common trees of east Bengal. The road hence was a good one, cut by
Sepoys across the dividing ranges, the first of which is not 500 feet
high. On the ascent bamboos abound, of the kind called Tuldah or
Dulloah, which has long very thin-walled joints; it attains no great
size, but is remarkably gregarious. On the east side of the range,
the road runs through soft shales and beds of clay, and
conglomerates, descending to a broad valley covered with gigantic
scattered timber-trees of jarool, acacia, _Diospyros, Urticeae,_ and
_Bauhiniae,_ rearing their enormous trunks above the bamboo jungle:
immense rattan-canes wound through the forest, and in the gullies
were groves of two kinds of tree-fern, two of _Areca, Wallichia_
palm, screw-pine, and _Dracaena._ Wild rice grew abundantly in the
marshes, with tal1 grasses; and _Cardiopteris_* [A remarkable plant
of unknown affinity; see Brown and Bennett, "Flora Java:" it is found
in the Assam valley and Chittagong.] covered the trees for upwards of
sixty feet, like hops, with a mass of pale-green foliage, and dry
white glistening seed-vessels. This forest differed from those of the
Silhet and Khasia mountains, especially in the abundance of bamboo
jungle, which is, I believe, the prevalent feature of the low hills
in Birmah, Ava, and Munnipore; also in the gigantic size of the
rattans, 1arger palms, and different forest trees, and in the scanty
undergrowth of herbs and bushes. I only saw, however, the skirts of
the forest; the mountains further east, which I am told rise several
thousand feet in limestone cliffs, are doubtless richer in
herbaceous plants.
The climate of Cachar partakes of that of the Jheels in its damp
equable character: during our stay the weather was fine, and dense
fogs formed in the morning: the mean maximum was 80 degrees, minimum
58.4 degrees.* [The temperature does not rise above 90 degrees in
summer, nor sink below 45 degrees or 50 degrees in January:
forty-seven comparative observations with Calcutta showed the mean
temperature to be 1.8 degrees lower at Silchar, and the air damper,
the saturation point being, at Calcutta 0.3791, at Silchar 0.4379.]
The annual rain-fall in 1850 was 111.60 inches, according to a
register kindly given me by Captain Verner. There are few mosquitos,
which is one of the most curious facts in the geographical
distribution of these capricious bloodsuckers; for the locality is
surrounded by swamps, and they swarm at Silhet, and on the river
lower down. Both on the passage up and down, we were tormented in our
canoes by them for eighty or ninety miles above Silhet, and thence
onwards to Cachar we were free.
Public-domain text, read in full here on John Shaqi.
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