Misfit stream
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A misfit stream (or underfit stream) is a stream that is far too small for its valley. Generally it is reasonable to expect a valley to be in proportion with the stream that occupies it. When a period of glaciation modifies the landscape by creating glacial troughs the rivers that occupy such valleys after the ice has retreated are not in proportion with the size of the valley. Given the scale of most glacial troughs almost all of them contain misfit streams.
[edit] Alternative causes
Misfit streams can also be caused by reductions in the discharge of the stream. Channel size responds rapidly to variations in discharge, but valley size responds over much longer timescales. Many causes of reduced discharges are possible. If misfit streams are widespread in an area climate change, particularly a reduction in precipitation is likely to be the cause. If a single river appears to be a misfit stream it may be as a result of anthropogenic interference through groundwater extraction or dam construction upstream.
[edit] See also
A misfit stream named Nose Creek in Calgary, Alberta:
[edit] References
Summerfield, M. A., (1991) Global Geomorphology Longman.
- U.S. Geological Survey, further clarification of a misfit stream.