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Geography

Which landform develops postglacially where freeze-thaw cycles promote solifluction?

A)Terraced slopes on gentle inclines
B)Deep, U-shaped hanging valleys
C)Sharp, arete-defined mountain ridges
D)Concentric kettle lakes and eskers

💡 Explanation

Terraced slopes form because repeated freeze-thaw weakens the soil, allowing solifluction, a soil creep process, to generate lobes and terraces. Therefore, gentle inclines yield terraced profiles rather than sharp ridges, which form through glacial erosion.

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