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
At Rampore I found the temperature of the ground, at three feet
depth, varied from 87.8 degrees to 89.8 degrees, being considerably
lower than that of the air (94.2 degrees), whilst that of a fine
ripening shaddock, into which I plunged a thermometer bulb, varied
little from 81 degrees, whether the sun shone on it or not. From this
place we made very slow progress south-eastwards, with a gentle
current, but against constant easterly winds, and often violent gales
and thunder-storms, which obliged us to bring up under shelter of
banks and islands of sand. Sometimes we sailed along the broad river,
whose opposite shores were rarely both visible at once, and at others
tracked the boat through narrow creeks that unite the many Himalayan
streams, and form a network soon after leaving their mountain valleys.
A few miles beyond Pubna we passed from a narrow canal at once into
the main stream of the Burrampooter at Jaffergunj: our maps had led
us to expect that it flowed fully seventy miles to the eastward in
this latitude; and we were surprised to hear that within the last
twenty years the main body of that river had shifted its course thus
far to the westward. This alteration was not effected by the gradual
working westwards of the main stream, but by the old eastern channel
so rapidly silting up as to be now unnavigable; while the Jummul,
which receives the Teesta, and which is laterally connected by
branches with the Burrampooter, became consequently wider and deeper,
and eventually the principal stream.
Nothing can be more dreary and uninteresting than the scenery of this
part of the delta. The water is clay-coloured and turbid, always
cooler than the air, which again was 4 degrees or 5 degrees below
that of Calcutta, with a damper atmosphere. The banks are of
stratified sand and mud, hardly raised above the mean level of the
country, and consequently unlike those bordering most annually
flooded rivers; for here the material is so unstable, that the
current yearly changes its course. A wiry grass sometimes feebly
binds the loose soil, on which there are neither houses nor
cultivation.
Ascending the Jummul (now the main channel of the Burrampooter) for a
few miles, we turned off into a narrower channel, sixty miles long,
which passes by Dacca, where we arrived on the 28th, and where we
were again detained for boats, the demand for which is rapidly
increasing with the extended cultivation of the Sunderbunds and
Delta. We stayed with Mr. Atherton, and botanised in the
neighbourhood of the town, which was once very extensive, and is
still large, though not flourishing. The population is mostly
Mahometan; the site, though beautiful and varied, is unhealthy for
Europeans. Ruins of great Moorish brick buildings still remain, and a
Greek style of ornamenting the houses prevails to a remarkable degree.
Public-domain text, read in full here on John Shaqi.
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