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About: Pendant bar     Goto   Sponge   NotDistinct   Permalink

An Entity of Type : yago:WikicatFloodplains, within Data Space : dbpedia.org associated with source document(s)

Type: yago:Floodplain109281914yago:Land109334396yago:Object100002684yago:PhysicalEntity100001930yago:Plain109393605yago:YagoGeoEntityyago:YagoPermanentlyLocatedEntityyago:WikicatFloodplains New Facet based on Instances of this Class

A pendant bar is a fluvial geomorphology term that is usually applied to large landforms created by large scale flooding events. Pendant bars are thin, sharp-crested deposits, and are typically made up of coarser sediment from the bed load. This type of bar is found on the downstream side of a weathering-resistant protrusion such as a large outcrop of bedrock, and is separated from the protrusion by a depression.