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Sediment transport is the movement of solid particles (sediment), typically due to a combination of gravity acting on the sediment, and the movement of the fluid in which the sediment is entrained.
Sedimentary processes include both transportation and sedimentation; they include the work of water, wind, ice and gravity. Transportation and deposition of sediments are governed by the laws of physics. Matter occurs in three phases: solid, liquid, and gaseous.
A streams gradient, discharge, and load are the three main factors that control what sediment a stream can carry.
Sediment moves from one place to another through the process of erosion. Erosion is the removal and transportation of rock or soil. Erosion can move sediment through water, ice, or wind. Water can wash sediment, such as gravel or pebbles, down from a creek, into a river, and eventually to that rivers delta.
Sediment is transported as suspended load (silt and clay held in the water column above the bottom by turbulence), bedload (sand, gravel and coarser material, like cobbles and boulders moved by rolling, sliding, and bouncing along the streambed), and dissolved load (products of chemical weathering of rocks carried in

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Deposition is the laying down of sediment carried by wind, flowing water, the sea or ice. Sediment can be transported as pebbles, sand and mud, or as salts dissolved in water. Salts may later be deposited by organic activity (e.g. as sea shells) or by evaporation.
Sedimentation is the deposition of rock fragments, soil, organic matter, or dissolved material that has been eroded, that is, has been transported by water, wind, ice, or gravity.
The agents involved in sediment transport are wave activity, tides, storm surges, nearshore currents, longshore drift, and rip currents. The primary process of sediment transport happens in four different ways: traction, saltation, suspension, and solution.

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