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 total breadth of the delta is 260 miles, from Chittagong to the
mouth of the Hoogly, divided longitudinally by the Megna: all to the
west of that river presents a luxuriant vegetation, while to the east
is a bare muddy expanse, with no trees or shrubs but what are planted
On the west coast the tides rise twelve or thirteen feet, on the
east, from forty to eighty. On the west, the water is salt enough for
mangroves to grow for fifty miles up the Hoogly; on the east, the sea
coast is too fresh for that plant for ten miles south of Chittagong.
On the west, fifty inches is the Cuttack fall of rain; on the east,
90 to 120 at Noacolly and Chittagong, and 200 at Arracan. The east
coast is annually visited by earthquakes, which are rare on the west;
and lastly, the majority of the great trees and shrubs carried down
from the Cuttack and Orissa forests, and deposited on the west coast
of the delta, are not only different in species, but in natural
order, from those that the Fenny and Chittagong rivers bring down
from the jungles.* [The Cuttack forests are composed of teak, Sal,
Sissoo, ebony, _Pentaptera, Buchanania,_ and other trees of a dry
soil, and that require a dry season alternating with a wet one.
These are unknown in the Chittagong forests, which have Jarool
(_Lagerstroemia_) _Mesua, Dipterocarpi,_ nutmegs, oaks of several
kinds, and many other trees not known in the Cuttack forests, and all
typical of a perennially humid atmosphere.]
We were glad to find at Noacolly that our observations on the
progression westwards of the Burrampooter (see chapter xxvii) were
confirmed by the fact that the Megna also is gradually moving in that
direction, leaving much dry land on the Noacolly side, and forming
islands opposite that coast; whilst it encroaches on the Sunderbunds,
and is cutting away the islands in that direction. This advance of
the fresh waters amongst the Sunderbunds is destructive to the
vegetation of the latter, which requires salt; and if the Megna
continues its slow course westwards, the obliteration of thousands of
square miles of a very peculiar flora, and the extinction of many
species of plants and animals that exist nowhere else, may ensue.
In ordinary cases these plants, etc., would take up their abode on
the east coast, as they were driven from the west; but such might not
be the case in this delta; for the sweeping tides of the east coast
prevent any such vegetation establishing itself there, and the mud
which the eastern rivers carry down, becomes a caking dry soil,
unsuited to the germination of seeds.
Public-domain text, read in full here on John Shaqi.
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