Channel Migration Zones Sample Clauses

Channel Migration Zones. Channel migration zones are located in low gradient stream reaches with banks composed primarily of unconsolidated alluvial material whose form is controlled by a balance between flow regime and sediment supply. Within these channels, bank stability is maintained by the roots of riparian vegetation and by LWD that is large enough to remain stable during winter storms. In alluvial channels, the removal of riparian vegetation and excess sediment supply increases bank erosion and causes channels to become wider and shallower with decreased pool habitat. Side channels often form in channel migration zones and provide quality fish habitat during high flows. Because these stream channels may migrate laterally in either direction during high flows, functional riparian zones should extend out to the valley walls to ensure proper riparian function for all potential channel locations.
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