Rivers of bangladesh essay
flows south, ending its independent existence as it joins the Padma. All the rivers of the former Nadia district (and of the present Kushtia District) were offshoots of the Padma (lower Ganges). Evidences show that the rivers Karatoya and Nagar have changed their courses in the past, while the Jamuna, lying on the eastern boundary of the district, is in fact a new channel of the Brahmaputra. As most of the rivers are navigable, they are used for carrying people and goods from one place to essays story lottery another and. This mighty network of four river systems flowing through the Bangladesh Plain drains an area of some.5 million square kilometers. (40) Chittagong (37) 100 Teesta Rangpur (70) 71 Following is a list of some of the major rivers of Bangladesh: Evening of Burigonga River, Dhaka, Bangladesh Ganges-Brahmaputra Delta edit Much of Bangladesh's geography is dominated by the Ganges-Brahmaputra Delta, but the term "Ganges" is not. The Jamuna River Essay.The Jamuna, river (Bangla: Jomuna) is one of the three main rivers of, bangladesh. It is the main channel of the Brahmaputra. Bangladesh, being a land of rivers, often falls victims to floods almost every year. Bad effects of floods: In spite of doing good floods often bring untold miseries to our country by damaging our crops and properties.
Rivers also provide fish, an important source of protein. The second system is the Padma-Ganges, which is divided into two sections: a 258-kilometer segment, the Ganges, which extends from the western border with India to its confluence with the Jamuna some 72 kilometers west of Dhaka, and a 126-kilometer segment, the Padma, which runs. The Karnaphuli Reservoir and Karnaphuli Dam are located in this area. In the Sadar subdivision, however, the general slope of the country is from west to east, and the main rivers fall into the Hurasagar, a tributary of the Jamuna. The Surma-Meghna, at 669 kilometers by itself the longest river in Bangladesh, is formed by the union of six lesser rivers. Apparently by 1830 the diversion of low-river flow down the new channel was complete. Again, melting of snow in the mountains and tidal bore of the sea create flood.
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