Karst lake
Lake formed as a result of the collapse of subterranean caves, especially in water-soluble rocks such as limestone, gypsum and dolomite
Karst lakes are formed as the result of a collapse of caves, especially in water-soluble rocks such as limestone, gypsum and dolomite. This process is known as karstification. They can cover areas of several hundred square kilometres.
Nº Q1734500 ★
Common · Knowledge
Karst lake
Lake formed as a result of the collapse of subterranean caves, especially in water-soluble rocks such as limestone, gypsum and dolomite
Karst lakes are formed as the result of a collapse of caves, especially in water-soluble rocks such as limestone, gypsum and dolomite. This process is known as karstification. They can cover areas of several hundred square kilometres.
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From Wikipedia
Karst lakes are formed as the result of a collapse of caves, especially in water-soluble rocks such as limestone, gypsum and dolomite. This process is known as karstification. They can cover areas of several hundred square kilometres. Their shallow lakebed is usually an insoluble layer of sediment so that water is impounded, leading to the formation of lakes. Many karst lakes only exist periodically, but return regularly after heavy rainfall.
Text: Wikipédia, CC BY-SA 4.0. ·
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