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Geography

Which process limits cave passage development beneath perched water tables?

A)Epiphreatic zone dissolution
B)Hypogenic speleogenesis rates
C)Vadose zone infiltration
D)Bathyal zone mixing

💡 Explanation

Epiphreatic zone dissolution facilitates passage enlargement at fluctuating water table levels because the alternating saturated and unsaturated conditions enhance chemical weathering. Therefore, it primarily shapes cave systems; rather than vadose infiltration, which primarily focuses on water delivery.

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