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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 ★

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Karst lake

Lake formed as a result of the collapse of subterranean caves, especially in water-soluble rocks such as limestone, gypsum and dolomite

Texto em inglês

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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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.

Texto: Wikipédia em inglês, CC BY-SA 4.0. ·

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