Avulsion (river)
Код 2369174
- ISBN: 978-5-5109-7084-5
Код 2369174
High Quality Content by WIKIPEDIA articles! In sedimentary geology and fluvial geomorphology, avulsion is the rapid abandonment of a river channel and the formation of a new river channel. Avulsions occur as a result of channel slopes that are much lower than the slope that the river could travel if it took a new course.
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