Teesta River

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Teesta River Bangladesh is a riverine country and Kurigram is a district where more than 16 rivers are criss- crossed. Even mighty Brahmaputra and flashy Teesta & Dharla rivers have flown through this district. So severe and flashy flood with a high scale of erosion is a common phenomenon near bank area of these rivers. Moreover sandy soil of the bank highly enhances the erosion. Not only that various small and high char forms at about the middle of the rivers for which river flow becomes one sided to the bank. That’s why these rivers flow with a higher thrust to the bank and its surrounded area. As a result each and every year thousands acre of paddy fields, homesteads, schools, college, mosque, local market engulfed into river. People of those localities are being poor to poorer by losing their valuable assets that washed out into the river. Especially sudden rise in water level in Teesta on 7 to 10th October 2009 caused a huge destruction to the erosion prone area at different places. Teesta river arises from the Cho Lhamu Lake at an average height of 5,330 metres (17,500 feet) above mean sea level in the majestic Himalayas. Teesta River merges with the rivulets, which arise in the Thangu, Yumthang and Donkia-La ranges. It then traverses the Rangpo town where it forms a boundary line between Sikkim and West Bengal up to Teesta Bazaar. It is at the Teesta suspension Bridge where the river meets the main tributary Rangeet River. At this level, the river changes its direction and flows southwards in West Bengal. The river meets the plains at Sevoke and then moves towards Jalpaiguri and then enters into Bangladesh at Kaligonj of Dimla Upazilla of Nilphamari district before surrendering itself to the Brahmaputra at Fulcherry in Bangladesh. The total length of the river is about 315 km. Teesta River is famous for river rafting. During the monsoons this humble river distends its banks; both in size and turbulence. Landslides in this region often dam up parts of the river in this season. Great changes have taken place in the course of the rivers and the adjoining areas, during the period since 1500 AD. Although positive evidence is lacking, similar changes can be assumed in the remoter past. The Teesta is one of the rivers that has changed over the years. .

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