Which outcome occurs when freeze-thaw cycles saturate the active layer in an area undergoing solifluction?

💡 Explanation

When freeze-thaw cycles saturate the active layer, solifluction occurs because water expands upon freezing, weakening soil cohesion and allowing gravity to pull saturated soil downhill as a viscous mass. Therefore, accelerated downslope soil movement results, rather than other listed which have dependencies on varying factors.

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