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Visitors on a walkway through a passage in Mammoth Cave.
Cave & Cavern Chemical Weathering

How Caves and Caverns Develop

Most large caves form when slightly acidic water slowly dissolves soluble rock, usually limestone, carving out underground passages over thousands of years.

Examples: Mammoth Cave (North America), Carlsbad Caverns (North America)

Formation timescale: Long (hundreds of thousands of years)

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The aftermath of the 1981 Winter Park, Florida sinkhole that collapsed part of a city block.
Sinkhole Chemical Weathering

How Sinkholes Form

A sinkhole forms when an underground void, usually created by the slow dissolution of soluble rock, finally loses enough support that the ground above it collapses.

Examples: Great Blue Hole (North America), Sima Humboldt (South America)

Formation timescale: Rapid (hours to years)

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Satellite image of limestone karst towers in the Trang An landscape, Vietnam.
Karst Landscape Chemical Weathering

Karst Landscapes and Limestone Erosion

Karst landscapes form when slightly acidic rainwater slowly dissolves soluble rock such as limestone, producing caves, sinkholes, disappearing streams, and sometimes dramatic rock towers.

Examples: Guilin Karst (China), Kras Plateau (Slovenia)

Formation timescale: Very Long (millions of years)

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