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River bank erosion along the Ganges in Malda and Murshidabad districts focusses on river bank erosion along the main channel of the Ganges in Malda and Mushidabad districts of West Bengal, India. Overview The Ganges is a long river carrying a huge discharge of 70,000 m 3 /s. However, the river bank erosion problems are restricted to a few places. Floods and erosion pose a serious problem in ...
[4] [5] The bank of the Ganges between Bhutni and Panchanandapur (both the places are marked on the map), is the area worst hit by left bank erosion, a major problem in the Malda area. [6] The ruins of Gauda, capital of several empires, is located in this area. [7] Note: The map alongside presents some of the notable locations in the area.
As of 2001 India census, [14] Old Malda Municipality had a population of 62,944. Males constitute 52% of the population and females 48%. Old Malda has an average literacy rate of 61%, higher than the national average of 59.5%: male literacy is 67%, and female literacy is 54%. In Old Malda, 15% of the population is under 6 years of age.
But Ruiz-Del Re said the city spent $1.8 million in federal pandemic relief funding in 2021-22 on its urban forestry. She said the one-time spending paid for the removal of mistletoe from 1,600 ...
After the rain ended on July 5, 2024, in Manawa, Wisconsin, spectators began to appear on the State 22 bridge over Little Wolf River to see the river's high water levels.
[2] [3] The bank of the Ganges between Bhutni and Panchanandapur (both the places are marked on the map), is the area worst hit by left bank erosion, a major problem in the Malda area. [4] The ruins of Gauda, capital of several empires, is located in this area. [5] Note: The map alongside presents some of the notable locations in the area.
The discharge of the spills far exceeds the original flow of the Cheslatta River, which has resulted in major erosion in the upper Cheslatta valley, with the scoured sediment being deposited in the lower valley. Large reservoir spills caused the lower Cheslatta River to avulse in 1961 and again in 1972, carving a new route to the Nechako River ...
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