Granular particle movement by fluids is the simplest concept of sediment transport. Gravity, river and stream flow, ice, wind, and estuary and ocean currents are the primary mechanisms by which sedimentary materials are transported.
Gravity acting on the sediment and/or the movement of the fluid where the sediment is entrained are two common causes of sediment transport, which is the transportation of solid particles (sediment). While organic silt is often detritus and decaying material, such as algae, mineral sediment is typically the result of erosion and weathering. Organic material, chemicals and contaminants, and mineral materials can all be found in transported sediment. Sediment load is an alternative term for sediment movement. agents transfer sediment Water Wind Glaciers Mass Wasting (gravity).
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