Why does the Brahmaputra in its Tibetan part have less silt, despite a longer course?
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Solution
The Brahmaputra river in its Tibetan part has less silt as it is a very dry and cold area.
The Brahmaputra river carries a smaller volume of water in Tibet.
After the river enters India, it flows through regions having very high rainfall.
In India, the Brahmaputra river carried a lot of silt and large volumes of water.
The river bed rises due to heavy deposition of silt by the Brahmaputra river.
Many riverine islands are formed by the river and the world’s largest riverine island – Majuli, is formed by the Brahmaputra river in Assam.
In Assam, along the entire length of the river, braided channels are formed.
Every year, widespread devastation is caused by the Brahmaputra river in Bangladesh and Indian state of Assam, due to floods caused by heavy rains.
The Brahmaputra rises near Mansarovar lake in Tibet, its source is very close to the sources of Sutlej and Indus river.
It flows parallel to the Himalayas in Eastward direction. It enters India in Arunachal Pradesh through a gorge. It makes a ‘U turn’ at Namcha Barwa and enters India.
In Arunachal Pradesh it is known as Dihang, it is joined by many tributaries like Dibang, Lohit and others to form Brahmaputra in Assam.