The Bagmati’s final sealing

The Bagmati River runs down from the Himalayan midhills surrounding Kathmandu Valley, entering India at the Sitamarhi District of Bihar. In Khagaria District, the river joins up with the Kosi River near Badla Ghat. The Bagmati's total catchment area of nearly 13,300 sq km is divided roughly evenly between India and Nepal, and its basin is among the world's most fertile regions, mainly due to the significant amount of silt carried by the river. The slope of the ground through which the river moves flattens out almost entirely once it enters the Gangetic plains, where the river's heavy silt load causes the Bagmati to meander.

South of the border, hydrologists divide the flow of the Bagmati into three distinct segments, each around 90 km in length. The lower reaches, although prone to overflow, are considered to be relatively stable, and hence were embanked during the mid-1950s in an attempt to solve the flood problems in that area. At that time, the upper and middle segments were left alone, with officials saying that it was unwise to embank the unstable portions of the river.

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