Karst topography is a geological formation shaped by the dissolution of a layer or layers of soluble bedrock, usually carbonate rock such as limestone or dolomite, but also in gypsum.[1] It has also been documented for weathering-resistant rocks, such as quartzite, given the right conditions.[2] This is an incomplete list of the major karst landscape areas of the world.
- ^ "Glossary of Cave and Karst Terms". Speleogenesis Information Network. Retrieved 2009-05-04.
- ^ Geomorphological Landscapes of the World.
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