Jaskinia Wielka Śnieżna
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Jaskinia Wielka Śnieżna
Jaskinia Wielka Śnieżna ("great snowy cave") is a limestone cave system in Mount Małołączniak in the Western Tatra Mountains, of the Carpathian Mountains System, in southern Poland. The cave is within Tatra National Park, Poland, Tatra National Park. With the length of , and vertical range of , it is the List of longest cave by country, longest, largest, and deepest cave in Poland. Morphology Wielka Śnieżna has five entrances: * Jaskinia Śnieżna ("snowy cave") – – discovered in 1959 * Jaskinia nad Kotlinami ("cave over the kettles") – – discovered in 1966, connected to Śnieżna in 1968 * Jasny Awen ("light aven") – – first explored in 1959, connected to Wielka Śnieżna in 1978 * Jaskinia Wielka Litworowa ("great angelica cave") – – connected to Wielka Śnieżna in 1995 * Jaskinia Wilcza ("gray wolf, wolf cave") – – discovered in 1996, connected to Wielka Śnieżna in 1999 They are connected by a complicated system of pitch (vertical space ...
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Limestone
Limestone is a type of carbonate rock, carbonate sedimentary rock which is the main source of the material Lime (material), lime. It is composed mostly of the minerals calcite and aragonite, which are different Polymorphism (materials science), crystal forms of calcium carbonate . Limestone forms when these minerals Precipitation (chemistry), precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly Dolomite (rock), dolomite, a closely related rock, which contains a high percentage of the mineral Dolomite (mine ...
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