In polar and alpine regions,the thawing and saturation of the upper layer of soil results in a slow downslope movement called

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The slow downslope movement resulting from thawing and saturation of the upper layer of soil in polar and alpine regions is called solifluction, and the landform it creates is known as a solifluction lobe. Mudflow, transitional slide, and lahars are all other types of mass wasting processes that occur in different types of environments.

In Polar and Alpine Regions,the Thawing and Saturation of the Upper