Solifluction results in the slow gradual bending of layered rock strata such as shales or slates.

Name: Solifluction results in the slow gradual bending of layered rock strata such as shales or slates.
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Solifluction is a type of mass wasting that involves the gradual movement of soil and regolith downhill due to the repeated freeze-thaw cycles. It can cause the deformation of the upper layers of soil and sediments, but not the bending of rock strata.

Solifluction Results in the Slow Gradual Bending of Layered Rock