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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 ]
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 ...
Limestone pavement on Orton Scar, Cumbria, England. Limestone pavements can be found in many previously glaciated limestone environments around the world. Notable examples are found in the Yorkshire Dales and Cumbria in Northern England, such as those above Malham Cove, on the side of Ingleborough, and above Grange-over-Sands. [3]
Limestone pavement – Natural karst landform consisting of a flat, incised surface of exposed limestone; Mesa – Elevated area of land with a flat top and sides, usually much wider than buttes; Mushroom rock – Naturally occurring rock whose shape resembles a mushroom; Natural arch – Arch-shaped natural rock formation
Karst formations and topography. Subcategories. This category has the following 12 subcategories, out of 12 total. C. Karst caves (5 C, 30 P) Karst formations of ...
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. All of them form in limestone settings.
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 ...