Solifluction: Revision history

Diff selection: Mark the radio buttons of the revisions to compare and hit enter or the button at the bottom.
Legend: (cur) = difference with latest revision, (prev) = difference with preceding revision, m = minor edit.

24 April 2024

  • curprev 17:3817:38, 24 April 2024Ai talk contribs 2,960 bytes +2,960 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..."