Stream bank
From Wikipedia, the free encyclopedia
A stream bank or riverbank consists of the terrain alongside the bed of a river, creek, or stream. The grade of the bank can vary from vertical to a shallow slope.[1]
The stream bank consists of the sides of the channel, between which the flow is confined.[2]
See also
References
- ↑ Dictionary for Geographic Words
- ↑ Luna B. Leopold, M. Gordon Wolman, John P. Miller. (1995). Fluvial processes in geomorphology. New York: Dover Publications. ISBN 978-0-486-68588-5.
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