Wind Erosion

Tree next to a cliff as examples of wind erosion.

Wind erosion. Transport of Particles by Wind Wind transports small particles such as silt and clay over great distances even halfway across a continent or an entire ocean basin. Rock formation in various location sculpted by wind erosion. Wind erosion is a natural process by which landforms are altered by the action of wind.

Wind erosion is a natural process that moves soil from one location to another by wind power. When the force of the wind is exerted on a land surface the soil moves. 1 Wind Erosion Overview The Agricultural Research Service has primary responsibility for erosion prediction research within the US.

In order to be transported the threshold velocity of the wind is needed. Wind affects the land through a process called wind erosion where wind breaks up land and then carries the debris like dirt and bits of rock to other places. It is a dynamic physical process where loose dry bare soils are transported by strong winds.

Obviously if the soil can be kept moist there is little danger of wind erosion. Describe how the size of sediment particles effects their movement during deflation. To keep beaches from eroding in the wind they too use windbreak fences and plant grasses that hold the sand in place slowing the erosion down.

Wind erosion is a widespread phenomenon causing serious soil degradation. The following principles and practices should be adopted for the management of eroded land wind. The extent of movement depends on the amount of soil moved depends on the size of the soil particles the cloudiness of the soil particles and the velocity of the wind wind velocity.

Control of Wind Erosion. It involves the detachment transportation and re-deposition of soil by wind. Wind is a more important erosional force in arid than humid regions.