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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 ]
Download as PDF; Printable version; ... Karst formations (12 C, 27 P) K. Karstologists (4 P) Pages in category "Karst" The following 45 pages are in this category ...
Download as PDF; Printable version; In other projects Wikimedia Commons; Wikidata item; Appearance. move to sidebar hide. ... Karst formations and topography ...
Global distribution of major outcrops of carbonate rocks (mainly limestone, except evaporites). The English word karst was borrowed from German Karst in the late 19th century, [6] which entered German usage much earlier, [7] to describe a number of geological, geomorphological, and hydrological features found within the range of the Dinaric Alps, stretching from the northeastern corner of ...
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Karstosphere (karst and Ancient Greek: σφαῖρα "sphere") is a geosphere of the karst processes; part of the lithosphere. [1] This is distinctly developed on continental platforms. It represents the Earth's broken shell occupying 35% of its surface and embracing vast areas of continents , as well as a considerable part their underwater ...
This is a list of karst springs. There are different types of karst springs , including inversacs (or estavelles), Vauclusian springs, vruljas, and others. All of them form in limestone settings.
Karst caves caves that have formed by dissolution of rock. They can be further sub− categorized into 4 specific types of karst they were formed within, Gypsum, Limestone, Quartzite, or Marble. Subcategories