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Physical Process

River Capture

Geomorphology

River capture, also called stream capture or piracy, occurs when a stream with greater erosive power, usually because it drains to a lower base level or has a steeper gradient, erodes headward until it breaches the divide separating it from a neighbouring drainage and diverts that neighbour headwaters into its own channel. The captured stream below the point of diversion is left as an underfit misfit stream in an oversized valley, a mismatch that is often the clearest field evidence a capture occurred. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/

Facts
Process Type
Fluvial 1
Timescale
Typically thousands to tens of thousands of years of headward erosion, though the final breach itself can occur within a single flood. 1
Timescale
Timescale (category)
Years 1
Timescale (category)
Thousands of Years 1
Connections

Caused By

Source River Capture (Wikipedia)
Sources
1. River Capture (Wikipedia)
Wikimedia FoundationView the Source
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