Braid bar
Depositional landform in a river which splits a channel / From Wikipedia, the free encyclopedia
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Braid bars, or mid-channel bars, are river landforms typically present in braided river channels. These formations have many names, including medial, longitudinal, crescentic, and transverse bars, as well as the more colloquial sandflat.[1] Braid bars are distinguished from point bars due to their presence in the middle of a flow channel, rather than along a bank of the river channel.