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Rainwater acidified by absorbed atmospheric carbon dioxide sinks through the joints and other discontinuities in the limestone upland's mass, dissolving the calcium carbonate that is the rock's main constituent.

Eventually the tiny initial conduits start to join and capture others, and discrete passages develop. The water emerges at a rising, resurgence or spring.

Read more: What_is_the_force_that_carves_out_underground_caves_from_limestone

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11y ago
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10y ago

The vast majority of the world's caves are in limestone, which is soluble in weakly acidic ground-water.

So the conditions for cave and other karst-feature development is the presence of a soluble rock (limestone and its metamorphic form, marble; also gypsum) in upland areas having a suitablly stable combination of geological, hydrological and long-term climate characteristics over the tens or hundreds of thousands of years it takes for caves to develop.

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Q: What conditions is a cave formed?
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how was the titan cave was formed


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