Which process primarily forms caves in limestone?

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Multiple Choice

Which process primarily forms caves in limestone?

Explanation:
Caves in limestone form mainly through chemical dissolution by slightly acidic groundwater. Rainwater picks up carbon dioxide from the air and soil, forming carbonic acid, which then percolates through fractures and pores in the limestone. As this water slowly circulates—especially below the water table—the calcite dissolves along those pathways, gradually enlarging them into caverns over long periods. This karst-like dissolution relies on sustained groundwater flow and chemical weathering, not rapid surface drainage or wind erosion. While hot water dissolution can occur in some settings, it isn’t the primary mechanism for most limestone caves.

Caves in limestone form mainly through chemical dissolution by slightly acidic groundwater. Rainwater picks up carbon dioxide from the air and soil, forming carbonic acid, which then percolates through fractures and pores in the limestone. As this water slowly circulates—especially below the water table—the calcite dissolves along those pathways, gradually enlarging them into caverns over long periods. This karst-like dissolution relies on sustained groundwater flow and chemical weathering, not rapid surface drainage or wind erosion. While hot water dissolution can occur in some settings, it isn’t the primary mechanism for most limestone caves.

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