Braided channels are characterized by multiple, active streams within a broad, low sinuosity channel. The smaller strands of streams diverge around sediment bars and then converge in a braiding pattern. Braided channels are dynamic, with strands moving within the channel. Braided channels are caused by sediment loads that exceed the capacity of stream transport. They are found downstream of glaciers and mountain slopes in conditions of high slope, variable discharge, and high loads of coarse sediment.
