After streams incise, they evolve through channel widening and adjustment of bank angle and bank shape. The rate of bank erosion and the influence of vegetation on the processes of adjustment on bank morphology are not well understood...
Zonge, L., S. Swanson, and T. Myers. 1996, Drought Year Changes in Streambank Profile on Incised Streams in the Sierra Nevada Mountains, Geomorphology, 15(1):47-56.

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