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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 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 ]
A polje, also called karst polje or karst field, [1] [2] [3] is a large flat plain found in karstic geological regions of the world, with areas usually in the range of 5–400 km 2 (2–154 sq mi). The name derives from the Slavic languages , [ 4 ] [ 5 ] where polje literally means 'field', whereas in English polje specifically refers to a ...
The cliffs of Duino and the gulf of Sistiana, Province of Trieste, Italy, seen from the Rilke Trail. The Karst Plateau or the Karst region (Slovene: Kras, Italian: Carso), also locally called Karst, is a karst plateau region extending across the border of southwestern Slovenia and northeastern Italy.
This is a list of karst springs. There are different types of karst springs, including inversacs (or estavelles), Vauclusian springs, vruljas, and others.
Pages in category "Karst" The following 45 pages are in this category, out of 45 total. This list may not reflect recent changes. ...
The subsurface phenomenon includes karst caves consisting of no less than 119 caves with stalactites and stalagmites, and underground rivers. Because of the uniqueness of its ecosystem, the 1993 International Union of Speleology proposed the Karst Area of the Sewu Mountains to be classed as a natural world heritage site.
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