Abstract
The Brahmaputra River has evolved in about two million years and rests on fractured pavements. Aggradation and degradation occur in alternate reaches of the river. The eroded sediment contributes to building the bars and islands within the river. This chapter presents a discussion of different channel processes that shape this huge river.
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Palaniappan, A.B. (2004). Channel Processes. In: Singh, V.P., Sharma, N., Ojha, C.S.P. (eds) The Brahmaputra Basin Water Resources. Water Science and Technology Library, vol 47. Springer, Dordrecht. https://doi.org/10.1007/978-94-017-0540-0_9
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DOI: https://doi.org/10.1007/978-94-017-0540-0_9
Publisher Name: Springer, Dordrecht
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