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 TimescaleTypically 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) Timescale (category) Connections
Caused By
Source River Capture (Wikipedia)
Shaped
Source Niger River (Wikipedia)
Sources
1. River Capture (Wikipedia)
Wikimedia FoundationLead section
Stream capture, river capture, river piracy or stream piracy is a geomorphological phenomenon occurring when a stream or river drainage system or watershed is diverted from its own bed, and flows down to the bed of a neighbouring stream.
- In Category: Physical Processes
- Caused By: Headward Erosion
View the Source Niger River (Wikipedia)
Wikimedia FoundationShaped: Niger River, Formation statement for target 290424Quote, Shaped: Niger River, Formation statement for target 290424
Over time upstream erosion by the lower Niger resulted in stream capture of the upper Niger by the lower Niger.
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