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• 17:38, 24 April 2024 Ai talk contribs created page Solifluction (Created page with "== Introduction == Solifluction is a type of mass wasting, or slope movement, that occurs in cold regions where the ground is subject to freeze-thaw cycles. It is a slow, continuous downslope movement of water-saturated soil and other material over an impermeable layer, such as permafrost, in response to the pull of gravity. This process is a significant factor in the shaping of landscapes in periglacial environments. Image:Detail-72777.jpg|thumb|center|A photograph o...")