Search results
Results From The WOW.Com Content Network
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 ...
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 ...
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.
Domica Cave in Slovak Karst (Slovakia.) The plains (plateaus) have many karst formations, such as karst pits with diameters of up to 250 m and depths of about 45 m, conical hills, blind and half-blind valley and dales. The subterranean karst is known for its deep vertical abysses, such as: Čertova diera (literally Devil's Hole; depth: 186 m)
The region is recognized as the world’s type area for karst landform development in the humid tropics and subtropics. The World Heritage Property of South China Karst is a serial property that includes seven karst clusters in four Provinces: Shilin Karst, Libo Karst, Wulong Karst, Guilin Karst, Shibing Karst, Jinfoshan Karst, and Huanjiang Karst.
Borenore's karst is surrounded by igneous rock that flowed from volcanic eruptions at nearby Mount Canobolas. [ 1 ] The 136-hectare (340-acre) reserve is situated 17 kilometres (11 mi) west of Orange , and is registered as a natural heritage site on the Register of the National Estate for its large diversity of karst morphological and ...
Large closed karst depressions are an important phenomenon on all continents, yet their analysis apart from and beyond dolines is rare. Assessing the potential of new knowledge, especially on the question of the genesis and evolution of large depressions, is very difficult.
The lake grows as ice thaws, which may result in the slumping of shorelines or submergence of vegetation, which is why thaw lakes in the boreal forest tend to be surrounded by "drunken trees". [19] It should be specified that "drunken trees" (also known as drunken forests) occur within Yedoma regimes. This feature is not present throughout all ...