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کارست

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کارست

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Also known as karst topography

thumb|Typical karst terrain of the Dinaric Alps thumb|Li River|Li Jiang fengcong (cone karst) in [[Guilin as part of the South China Karst]] thumb|Karst formation of the Serra de Tramuntana Karst () is a topography formed from the dissolution of soluble carbonate rocks such as limestone and dolomite. It is characterized by features like poljes above and drainage systems with sinkholes and caves underground. There is some evidence that karst may occur in more weathering-resistant rocks such as quartzite given the right conditions.

AI overview

Karst is a type of landscape created when soluble rocks like limestone and dolomite dissolve away, producing distinctive features including underground caves and sinkholes along with surface valleys called poljes. This terrain matters because it creates unique environments that affect how water flows underground and shapes the geography of many regions around the world.

AI-generated from the Wikipedia summary — may contain errors.

Wikidata facts

Subclass of
landform
Show 6 more facts
studied by
karstology
topic's main category
Category:Karst
native label
Karst
Commons category
Karst
on focus list of Wikimedia project
Wikipedia:Vital articles/Level/4
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