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Physical Process

Headward Erosion

Geomorphology

The lengthening of a stream valley upslope as erosion at its uppermost point cuts back into previously unchannelled terrain, extending the drainage network over time. It is a principal mechanism of river piracy, by which one stream's headward growth can intercept and divert the flow of a neighboring drainage basin.

Facts
Process Type
Fluvial 1
Connections

Caused By

Causes

Source Knickpoint Retreat (Wikipedia)
Source River Capture (Wikipedia)
Sources
1. Headward erosion, Wikipedia
Lead section, third sentence
Quote, Lead section, third sentence
Headward erosion is a fluvial process of erosion that lengthens a stream, a valley or a gully at its head and also enlarges its drainage basin.
View the Source
Knickpoint Retreat (Wikipedia)
Wikimedia FoundationCauses: Knickpoint RetreatView the Source
River Capture (Wikipedia)
Wikimedia FoundationCauses: River CaptureView the Source
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