It is called wind erosion .
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The lifting and removal of fine sediments by wind is called aeolian transport. This process involves the suspension, saltation, and surface creep of particles by the wind, leading to the transportation of sediments over distances. Aeolian transport is an important geomorphic process in shaping landscapes like deserts and coastal dunes.
The lifting and removal of fine sediments by wind is called "deflation." This process occurs when wind energy is able to overcome the cohesive forces holding the sediment particles together, causing them to be lifted and carried away. Deflation is a common process in arid and semi-arid environments where vegetation cover is sparse.
Loess
Sediments can be picked up by wind, and water.
Erosion by wind can lead to the removal of fine soil particles, decrease soil fertility, and cause loss of topsoil. It can also contribute to the formation of sand dunes in desert regions. Overall, wind erosion can have negative impacts on soil quality and ecosystem health.
By water or wind