Solifluction is an important mass wasting process in areas of permafrost.

Name: Solifluction is an important mass wasting process in areas of permafrost.
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Solifluction is a mass wasting process that occurs in areas of permafrost where the upper layer of soil thaws during the summer months and becomes saturated with water, causing it to become unstable and flow downhill. It is a common feature in polar and subpolar regions and can result in significant landscape changes over time.

Solifluction Is an Important Mass Wasting Process in Areas of Permafrost