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About: River channel migration     Goto   Sponge   NotDistinct   Permalink

An Entity of Type : yago:WikicatRivers, within Data Space : dbpedia.demo.openlinksw.com associated with source document(s)

Type: yago:BodyOfWater109225146yago:PhysicalEntity100001930yago:YagoGeoEntityyago:YagoPermanentlyLocatedEntityElectionyago:River109411430yago:Stream109448361yago:Thing100002452yago:WikicatRivers New Facet based on Instances of this Class

River channel migration is the geomorphological process that involves the lateral migration of an alluvial river channel across its floodplain. This process is mainly driven by the combination of bank erosion of and point bar deposition over time. When referring to river channel migration, it is typically in reference to meandering streams. In braided streams, channel change is driven by sediment transport. It has been proposed that lateral migration is a particularly dominant erosive process in savanna landscapes.