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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 ...
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 Nambung River flows underground into a karst system bounding the eastern edge of the Nambung Wetlands, within Nambung National Park. Features associated with the wetlands include salt lakes, swamps, lagoons and dunal damplands. Most lagoons and lakelets in the area are isolated from the sea and from surface creek drainage, being fed by ...
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.
Thanks to the research work of the Serbian geographer Jovan Cvijić (1865–1927), the protégé of Albrecht Penck (the Nestor of the Vienna School of Physical Geography), the word uvala – like the words 'karst', 'dolina' or 'polje', popular terms of the Dinarides – became an established international standard.
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The general morphology (shape, depth, circumference) is variable, with some thaw lakes oriented, meaning they are generally elongated in a specific direction. Though their formation mechanism has not been definitively proven, it is believed to be related to the prevailing winds or storms. [ 15 ]