Larger sediments that roll, bounce, or slide over the bottom are referred to as suspended load, dissolved load, and bed load.
Water flow is slowest at the bottom and edges and quickest towards the surface and in the middle of the stream because friction along the stream bed reduces flow velocity. The friction between the water and the air actually causes the velocity just below the surface to be slightly higher than it is just at the surface.
The term "suspended load" describes the silt that streams and rivers transport in the water column but does not directly reach the bed surface for extended periods of time.
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