Most streams carry the largest part of their load as bed load.

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Most streams carry the largest part of their load as suspended load, which is composed of fine sediment particles that are carried within the water column. Bed load, on the other hand, refers to larger sediment particles that move along the streambed by rolling, sliding, or bouncing. While bed load can be an important component of a stream's sediment load, it typically constitutes a smaller proportion of the total load than suspended load.

Most Streams Carry the Largest Part of Their Load as Bed