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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.
We proceeded up the Burrampooter, crossing it obliquely; its banks were on the average five miles apart, and formed of sand, without clay, and very little silt or mud: the water was clear and brown, like that of the Jheels, and very different from that of the Jummul. We thence turned eastwards into the delta of the Soormah, which we traversed in a north-easterly direction to the stream itself.
Thomson for the Khasia mountains Mahanuddy river Vegetation of banks Maldah Alligators Rampore-Bauleah Climate of Ganges Pubna Jummul river Altered course of Burrampooter and Megna Dacca Conch shells Saws Cotton muslins Fruit Vegetation Elevation Rose of Bengal Burrampooter Delta of Soormah river Jheels Soil Vegetation Navigation Mosquitos Atmospheric pressure Effects of geological changes Imbedding of plants Teelas or islets Chattuc Salubrious climate Rains Canoes Pundua Mr.
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