- Meander cutoff
-
A meander cutoff occurs when a meander bend in a river is breached by a chute channel that connects the two closest parts of the bend. This causes the flow to abandon the meander and to continue straight downslope. Cutoffs are a natural part of the evolution of a meandering river, and have also been used to artificially shorten the length of meandering rivers for navigation.
In March, 1876, a cutoff formed suddenly across the neck of a meander in the Mississippi River near Reverie, Tennessee, shortening the river's course and leaving the town connected to Arkansas but across the new river channel from the rest of Tennessee.
River morphology Large-scale features Alluvial rivers Meander • Meander cutoff • Point bar • Cut bank • Riffle • Stream pool • Braided river • Bar (river morphology) • Anabranch • River bifurcation • River channel migration • Oxbow lake • Floodplain • Riparian corridor • Avulsion (river) • Mouth bar • Thalweg • Channel patternBedrock river Bedforms Regional processes Mechanics Playfair's Law • Hack's law • Sediment transport • Water erosion • Deposition (geology) • Exner equationCategory · Portal This geomorphology article is a stub. You can help Wikipedia by expanding it.