Online Encyclopedia

MEGHNA

Online Encyclopedia
Originally appearing in Volume V18, Page 78 of the 1911 Encyclopedia Britannica.
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MEGHNA  , a

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river of India . It forms, in the
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lower
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part of its course, the
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great estuary of the Bengal delta, which conveys to the sea the main
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body of the waters of the Ganges and the
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Brahmaputra, which unite at Goalanda in Faridpur
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district . The
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united waters, turbid and of great
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depth, are sometimes split into
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half a dozen channels by sand-banks, sometimes spread into a wide
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sheet of
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water . The river enters the sea by four
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principal mouths, enclosing the three large islands of Dakshin Shahbazpur, Hatia and Sandwip . It is navigable by native boats and river steamers all the
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year; but the navigation is difficult and some-times dangerous on account of shifting sand-banks and snags, and boisterous weather when the monsoon is blowing . The most favourable season is between November and
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February . AlIuvion and diluvion are constantly taking place, especially along the seaboard, and in
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Noakhali district the
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land is said to have made rapid advance on the sea; while the islands fringing the mouth are annually being cut away and redeposited in fresh shapes . The
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regular rise of the tide is from To to 18 ft., and at springs the sea rushes up in a dangerous
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bore . It is greatest at the time of the biennial equinoxes, when navigation is sometimes impeded for days together . The tidal
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wave advances like a wall topped with foam of the height of nearly 20 ft., and at the
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rate of 15 M. an
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hour; in a few minutes it is past, and the river has changed from ebb to flood tide . A still greater danger is the " storm wave " which occasionally sweeps up the Meghna under a cydone .

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