List Of Caves In Slovenia
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List Of Caves In Slovenia
The following article is a list of caves in Slovenia. About 43% of Slovenian territory is of karst nature and over 14,000 caves (2021) are known in Slovenia. List of caves by number of visitors The following show caves were the most visited in 2008 (ordered by the number of visitors): #Postojna Cave: 548,424 visitors #Å kocjan Caves: 100,299 visitors #Hell Cave: 13,638 visitors # Predjama Cave: 6,133 visitors #Cross Cave: 4,935 visitors # Mayor Cave: 4,008 visitors # Pivka Cave and Black Cave: 3,509 visitors List of longest and deepest caves It includes all the caves in the Slovenian cave registry, at least 1,000 m long and at least 300 m deep (March 2023). The list is sorted on a cave score, obtained as a sum of normalized length (divided by the length of the longest cave, multiplied by 100) and depth (divided by the depth of the deepest cave times 100) - maximal possible score would be 200. See also * List of caves * Speleology References External links Online Cave ...
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Slovenia
Slovenia ( ; sl, Slovenija ), officially the Republic of Slovenia (Slovene: , abbr.: ''RS''), is a country in Central Europe. It is bordered by Italy to the west, Austria to the north, Hungary to the northeast, Croatia to the southeast, and the Adriatic Sea to the southwest. Slovenia is mostly mountainous and forested, covers , and has a population of 2.1 million (2,108,708 people). Slovenes constitute over 80% of the country's population. Slovene, a South Slavic language, is the official language. Slovenia has a predominantly temperate continental climate, with the exception of the Slovene Littoral and the Julian Alps. A sub-mediterranean climate reaches to the northern extensions of the Dinaric Alps that traverse the country in a northwest–southeast direction. The Julian Alps in the northwest have an alpine climate. Toward the northeastern Pannonian Basin, a continental climate is more pronounced. Ljubljana, the capital and largest city of Slovenia, is geogr ...
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Sistem Migovec
The Migovec System ( sl, Sistem Migovec) is a and Alpine cave system within Mount Tolmin Migovec () in the Municipality of Tolmin in northwestern Slovenia. The mountain and the cave system are part of Triglav National Park. The combined system is the longest known cave in the country, followed by the Postojna Cave System (). Entrances The entrances include: * Chough Cave () (M2), first explored in 1972, and the highest entrance to the system at 1861 m above sea level *M16, first explored in 1982 *Torn T-Shirt () (M18), first explored in 1994 *Gardeners' World (), first explored in 2000 *Fairy Cave (), first explored in 2008 *Primadona, first explored in 1999 *Monatip, first explored in 2007 Exploration The majority of exploration has been carried out by the Caving Section of the Tolmin Mountaineering Club (), joined since 1994 by Imperial College Caving Club. Chough Cave (M2), Torn T-Shirt (M18), and M16 were connected together in 1996 to form the initial Migovec System, ...
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Caves Of Slovenia
A cave or cavern is a natural void in the ground, specifically a space large enough for a human to enter. Caves often form by the weathering of rock and often extend deep underground. The word ''cave'' can refer to smaller openings such as sea caves, rock shelters, and grottos, that extend a relatively short distance into the rock and they are called ''exogene'' caves. Caves which extend further underground than the opening is wide are called ''endogene'' caves. Speleology is the science of exploration and study of all aspects of caves and the cave environment. Visiting or exploring caves for recreation may be called ''caving'', ''potholing'', or ''spelunking''. Formation types The formation and development of caves is known as ''speleogenesis''; it can occur over the course of millions of years. Caves can range widely in size, and are formed by various geological processes. These may involve a combination of chemical processes, erosion by water, tectonic forces, microorganisms ...
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Ljubljana Cave Exploration Society (DZRJL)
Ljubljana (also known by other Ljubljana#Name, historical names) is the Capital city, capital and largest city of Slovenia. It is the country's cultural, educational, economic, political and administrative center. During antiquity, a Roman city called Emona stood in the area. Ljubljana itself was first mentioned in the first half of the 12th century. Situated at the middle of a trade route between the northern Adriatic Sea and the Danube region, it was the historical capital of Carniola, one of the Slovenes, Slovene-inhabited parts of the Habsburg monarchy. It was under House of Habsburg, Habsburg rule from the Middle Ages until the dissolution of the Austria-Hungary, Austro-Hungarian Empire in 1918. After World War II, Ljubljana became the capital of the Socialist Republic of Slovenia, part of the Socialist Federal Republic of Yugoslavia. The city retained this status until Slovenia became independent in 1991 and Ljubljana became the capital of the newly formed state. Name The ...
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Speleology
Speleology is the scientific study of caves and other karst features, as well as their make-up, structure, physical properties, history, life forms, and the processes by which they form (speleogenesis) and change over time (speleomorphology). The term ''speleology'' is also sometimes applied to the recreational activity of exploring caves, but this is more properly known as ''caving'', ''potholing'' (British English), or ''spelunking''. Speleology and caving are often connected, as the physical skills required for ''in situ'' study are the same. Speleology is a cross-disciplinary field that combines the knowledge of chemistry, biology, geology, physics, meteorology, and cartography to develop portraits of caves as complex, evolving systems. History Before modern speleology developed, John Beaumont wrote detailed descriptions of some Mendip caves in the 1680s. The term speleology was coined by Émile Rivière in 1890. Prior to the mid-nineteenth century the scientific valu ...
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List Of Caves
This is a list of caves of the world that have articles or that are properly cited. They are sorted by continent and then country. Caves which are in overseas territories on a different continent than the home country are sorted by the territory's continent and name. Africa File:Cango Caves, Western Cape (6253225986).jpg, The Cango caves in western cape. File:African cave paintings.jpg, African cave paintings. File:Lithic Industries at Blombos Cave, Southern Cape, South Africa (c. 105 – 90 Ka).jpg, Lithic Industries at Blombos Cave, Southern Cape, South Africa. File:Wonder Caves Praying Mary.JPG, Wonder Caves Praying Mary. Algeria * Aïn Taïba * Anou Achra Lemoun * Anou Boussouil * Anou Ifflis * Anou Timedouine * Gueldaman caves * Ghar Boumâaza * Grotte de Cervantes * Kef Al Kaous * Rivière De La Tafna Botswana * Gcwihaba * Rhino Cave Cameroon * Gouffre de Mbilibekon * Grottes de Linté * Grotte de Loung * Grotte de Mfouda * Grotte Fovu
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Weaver Cave
Weaver Cave ( sl, Tkalca jama), also known as Inlet Cave (), is a long ponor cave in southwest Slovenia. It runs from the west (downstream) side of the Rak Å kocjan Valley, where it has two entrances, and continues into Planina Cave. It is traversed by Rak Creek, part of the Ljubljanica source system. It thus forms part of the hydrological connection between Cerknica Polje and Planina Polje. Due to sumps, the stream of the Rak is very difficult to follow and was explored by divers only in 1974, when the majority of the cave was discovered in the course of a rescue expedition, and in August 2012. The cave was named after a stalagmite reminiscent of a weaver. An old story says that he was turned to stone because he worked on Sunday, the Lord's Day. The first description of Weaver Cave was published in 1687 by Johann Weikhard von Valvasor in the ''Philosophical Transactions of the Royal Society''. He also published an engraving of it. The cave has also been depicted by other artis ...
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Planina Cave
Planina Cave ( sl, Planinska jama), formerly also Little Castle Cave () after Little Castle in the vicinity of its entrance, is one of the longest Slovenian active caves. It is a huge tunnel and the subterranean bed of the Unica River. It is located in Inner Carniola. Five hundred meters from the entrance into the cave is a confluence of two underground rivers: the Pivka River, flowing from the Postojna Polje through Postojna Cave, and the Rak River, flowing to Planina Cave through Weaver Cave from Rak Å kocjan. This is one of the largest confluences of subterranean rivers in Europe. Entrance into the cave is at the southwestern part of Planina Polje in the gable end valley below 65 high rocks. The length of the cave is . It has been shown by water tracing that there is a connection between the systems of Planina Cave and Postojna Cave, and the administration of Postojna Cave estimates the connection will also be explored by cavers. The length of the joint system would be ov ...
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ÄŒehi 2 Cave
ÄŒehi 2 on Rombonski podi is the deepest sinkhole in Slovenia and the 13th deepest cave in the world. It is 1505 meters deep and 5536 meters long. There is a siphon at the bottom. The entrance is located 2033 meters above the sea level. The cave was discovered in 1991. The depth of the cave makes it very popular for Slovenian and foreign cave expeditions. See also *List of caves in Slovenia The following article is a list of caves in Slovenia. About 43% of Slovenian territory is of karst nature and over 14,000 caves (2021) are known in Slovenia. List of caves by number of visitors The following show caves were the most visited in ... * List of deepest caves References External links3D model jam na Kaninskih podihKras na Kaninskih podih

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Migovec System
The Migovec System ( sl, Sistem Migovec) is a and Alpine cave system within Mount Tolmin Migovec () in the Municipality of Tolmin in northwestern Slovenia. The mountain and the cave system are part of Triglav National Park. The combined system is the longest known cave in the country, followed by the Postojna Cave System (). Entrances The entrances include: * Chough Cave () (M2), first explored in 1972, and the highest entrance to the system at 1861 m above sea level *M16, first explored in 1982 *Torn T-Shirt () (M18), first explored in 1994 *Gardeners' World (), first explored in 2000 *Fairy Cave (), first explored in 2008 *Primadona, first explored in 1999 *Monatip, first explored in 2007 Exploration The majority of exploration has been carried out by the Caving Section of the Tolmin Mountaineering Club (), joined since 1994 by Imperial College Caving Club. Chough Cave (M2), Torn T-Shirt (M18), and M16 were connected together in 1996 to form the initial Migovec System, ...
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Black Cave
Black is a color which results from the absence or complete absorption of visible light. It is an achromatic color, without hue, like white and grey. It is often used symbolically or figuratively to represent darkness. Black and white have often been used to describe opposites such as good and evil, the Dark Ages versus Age of Enlightenment, and night versus day. Since the Middle Ages, black has been the symbolic color of solemnity and authority, and for this reason it is still commonly worn by judges and magistrates. Black was one of the first colors used by artists in Neolithic cave paintings. It was used in ancient Egypt and Greece as the color of the underworld. In the Roman Empire, it became the color of mourning, and over the centuries it was frequently associated with death, evil, witches, and magic. In the 14th century, it was worn by royalty, clergy, judges, and government officials in much of Europe. It became the color worn by English romantic poets, businessmen ...
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Karst
Karst is a topography formed from the dissolution of soluble rocks such as limestone, dolomite, and gypsum. It is characterized by underground drainage systems with sinkholes and caves. It has also been documented for more weathering-resistant rocks, such as quartzite, given the right conditions. Subterranean drainage may limit surface water, with few to no rivers or lakes. However, in regions where the dissolved bedrock is covered (perhaps by debris) or confined by one or more superimposed non-soluble rock strata, distinctive karst features may occur only at subsurface levels and can be totally missing above ground. The study of ''paleokarst'' (buried karst in the stratigraphic column) is important in petroleum geology because as much as 50% of the world's hydrocarbon reserves are hosted in carbonate rock, and much of this is found in porous karst systems. Etymology The English word ''karst'' was borrowed from German in the late 19th century, which entered German much earlier ...
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