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← GeographyWhich 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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