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- W4226062747 abstract "The Yangtze River originates from the Tuotuo on the southwestern slopes of the snow-draped Geladandong Mountains on the Tibetan Plateau at about 6000 m elevation. The Yangtze Basin includes a complex variety of geological units, primarily sedimentary rocks of different ages. Limestone and terrigenous sedimentary rocks of Palaeozoic age with granite constitute the Upper Yangtze drainage basin. The Sichuan Basin is surrounded by a complex of mountains framed by distinctive tectonic units. Erosion and deposition patterns pre- and post-dam changing sediment load is a useful criterion for assessing the erodibility of a river channel. An anabranching channel pattern typifies the Lower Yangtze River flowing between a series of low hills and Pleistocene river terraces. The chapter examines the relationship between sediment transport and environmental challenge from recent intensive human modification, chiefly represented by the ongoing Three Gorges project and South–North Water Transfer project." @default.
- W4226062747 created "2022-05-05" @default.
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- W4226062747 date "2022-04-01" @default.
- W4226062747 modified "2023-10-13" @default.
- W4226062747 title "Dynamic Hydrology and Geomorphology of the Yangtze River" @default.
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- W4226062747 doi "https://doi.org/10.1002/9781119412632.ch23" @default.
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