Erosion and deposition work together to form sand dunes primarily through the processes of deflation and the subsequent deposition of sand.
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Erosion through Deflation: Wind plays a significant role in the erosion process, particularly in arid and semi-arid regions. Deflation occurs when the wind picks up loose sand and other small particles from the ground, resulting in the removal of surface materials. This action can create depressions in the landscape and reduce the overall elevation of the surface in those areas.
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Deposition: After the sand particles are eroded and carried by the wind, they are eventually deposited when the wind's velocity decreases or when it encounters an obstacle, such as vegetation, rocks, or other landforms. This deposition occurs as the wind loses the energy necessary to carry the sediment, causing the sand to accumulate.
As these processes continue, sand accumulates over time in specific areas, leading to the formation of sand dunes. The shape and size of the dunes can vary based on factors like wind direction, sand supply, and the presence of vegetation, which can stabilize the sand and promote dune growth.
In summary, erosion (through deflation) removes sand and sediment, while deposition allows that material to accumulate in new locations, leading to the development of sand dunes.