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.

• Which outcome occurs when regional dust storms deposit loess?
• Which effect causes desertification on the leeward side of mountain ranges?
• Which landscape outcome develops because subsurface limestone dissolution accelerates?
• Which mechanism causes stream channel sinuosity in meandering river systems despite continuous downslope flow?
• Which process limits the maximum magnitude of earthquakes along a transform fault zone?
• Which process limits nutrient transport rates in stratified subtropical gyres containing a strong thermocline?