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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 ]
Karst (/ k ɑːr s t /) is a topography formed from the dissolution of soluble carbonate rocks such as limestone and dolomite. It is characterized by features like ...
Karst lakes are found in the area around the Harz Mountains of Germany (e. g. the Juessee and the Bauerngraben in the South Harz Karst Landscape Biosphere Reserve, an episodic karst lake on the Karst Trail), [1] in South Germany (e.g. the Eichener See), in France in the region of Quercy, in Estonia the Tudre and the region of Salajõe, [2] in Slovenia (e. g. the Cerkniško jezero), in ...
Kampong Danau (Malay: Kampung Danau), simply known as Danau, is a coastal village in Tutong District, Brunei, about 21 kilometres (13 mi) from the district town Pekan Tutong. It has a total area of 6.5023 square kilometres (2.5106 sq mi); [3] the total population was 1,072 in 2016. [a] It is one of the villages within Mukim Telisai. [4]
This is a list of karst springs. There are different types of karst springs, including inversacs (or estavelles), Vauclusian springs, vruljas, and others.
The Sangkulirang-Mangkalihat Karst is a karstique area in Sub Kelay, Biatan, Talisayan, Batu Putih, and Biduk-biduk Berau districts of East Kalimantan province on the island of Borneo in Indonesia. It covers an area of 105,000 hectares, including the Mangkalihat Peninsula .
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
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