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Physical Process

River Avulsion

Geomorphology

The sudden abandonment of a river's existing channel for a new course across its floodplain, typically triggered when sediment deposition raises the existing bed until it becomes easier for floodwater to break out and carve a new, lower-gradient path. Avulsion can relocate a river's course by many kilometres within a single flood season and has repeatedly reshaped major deltas, including the Yellow River's, whose mouth has shifted across a wide span of coastline over recorded history.

Facts
Process Type
Fluvial 1
Connections

Caused By

Sources
1. River Avulsion (Wikipedia)
Wikimedia FoundationIntroduction
Quote, Introduction
In sedimentary geology and fluvial geomorphology, avulsion is the process by which flow is diverted out of an established river channel and into a new course via a bifurcation, or splitting of the channel.
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