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Which risk dramatically increases when groundwater recharge rates decline within karst regions overlying soluble carbonate rocks?

A)Accelerated sinkhole formation likelihood
B)Increased likelihood glacial advancement
C)Volcanic eruption frequency amplification
D)Decreased surface temperature stability

💡 Explanation

Decreased groundwater recharge amplifies dissolution of carbonate rock, causing increased sinkhole formation, because chemical weathering is heightened. Solution Widening creates voids; therefore, sinkhole risk increases rather than glacial change, because karst systems are independent of ice formation.

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