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Geography

Which consequence results when intense freeze-thaw cycles affect loess deposits?

A)Increased soil particle consolidation occurs
B)Solifluction and slope instability increase
C)Cementation of loess is accelerated
D)Reduced infiltration lowers plant support

💡 Explanation

Increased solifluction occurs because frost-thaw action reduces cohesion in loess soils via heaving. This destabilization allows mass wasting. Therefore, failures increase gradually in colder areas rather than consolidation under increasing overburden.

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