The steep topography along the Yarlung-Tsangpo River ( (Tibetan: ཡར་ཀླུངས་གཙང་པོ་, Wylie: yar kLungs gTsang po) is created due to the interplay between the forces of tectonics and powerful river erosion, which in turn leads to large landslides.
This is the conclusion drawn by Isaac J. Larsen and David R. Montgomery from the University of Washington (presented online May 27, 2012 in Nature Geoscience) after quantifying landslide erosion rates in the eastern Himalaya.
They closely observed an area of the 150-mile Tsangpo Gorge in southeastern Tibet, where the Tsangpo plunges more than 6,500 feet (1.25 miles), before entering India to form Brahmaputra River and flow into Bay of Bengal through the Ganges River delta.