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Abrasion in a stream or river channel occurs when the sediment carried by a river scours the bed and banks, contributing significantly to erosion. In addition to chemical weathering and the physical weathering of hydraulic action , freeze-thaw cycles (see frost weathering ), and more, there is a suite of processes which have long been considered to contribute significantly to bedrock channel erosion include plucking , abrasion (due to both bedload and suspended load ), solution , and cavitation . [5] [6]