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Bystrianska Cave
Bystrianska Cave is a limestone cave located on the southern slopes of the Nizke Tatry Mountains, along the road towards Banska Bystrica, at the southern edge of the town of Bystrá, in the Brezno District, Banskobystrický region, in Slovakia. History The old parts of the cave have been known already in the prehistoric times. Though the precipice Peklo the new parts have been discovered by E. and A. Hollmann and J. Kovalčík in 1926. In 1951 the Mostárenské Hall was discovered. The lower entrance to the cave was opened in 1932. The Old and New Cave were connected by J. Majko and J. Vytřísalová together with their colleagues in 1955. About of the cave has been made public in 1968. The Lower Guerilla Hall and some other parts of the cave have been used for speleotherapy since 1971. Description The cave consists primarily of dark limestone rocks of the middle trias, formed in tectonic Tectonics (; ) are the processes that control the structure and properties of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals 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, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tectonic
Tectonics (; ) are the processes that control the structure and properties of the Earth's crust and its evolution through time. These include the processes of mountain building, the growth and behavior of the strong, old cores of continents known as cratons, and the ways in which the relatively rigid plates that constitute the Earth's outer shell interact with each other. Tectonics also provide a framework for understanding the earthquake and volcanic belts that directly affect much of the global population. Tectonic studies are important as guides for economic geologists searching for fossil fuels and ore deposits of metallic and nonmetallic resources. An understanding of tectonic principles is essential to geomorphologists to explain erosion patterns and other Earth surface features. Main types of tectonic regime Extensional tectonics Extensional tectonics is associated with the stretching and thinning of the crust or the lithosphere. This type of tectonics is found ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Western Carpathians
The Western Carpathians are a mountain range and geomorphological province that forms the western part of the Carpathian Mountains. The mountain belt stretches from the Low Beskids range of the Eastern Carpathians along the border of Poland with Slovakia toward the Moravian region of the Czech Republic and the Austrian Weinviertel. In the south the North Hungarian Mountains cover northern Hungary. The area of the Western Carpathians comprises about 70,000 km². The highest elevation is the Gerlachovský štít (2,655m). Geographical definition Most of the perimeter of the Western Carpathians is quite sharply defined by valleys. To the northwest and north they are separated from the Bohemian Massif by the Forecarpathian Lowland and the Lesser Poland Upland; to the west the Moravian Gate leads over to the Sudetes. To the south the mountain chain falls away towards the Pannonian Plain, a large plain situated between the Alps, the Dinaric Alps, and the main mass of the Ea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone Caves
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals 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, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limestone co ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
World Heritage Sites In Slovakia
The United Nations Educational, Scientific and Cultural Organization (UNESCO) World Heritage Sites are places of importance to cultural or natural heritage as described in the UNESCO World Heritage Convention, established in 1972. Cultural heritage consists of monuments (such as architectural works, monumental sculptures, or inscriptions), groups of buildings, and sites (including archaeological sites). Natural features (consisting of physical and biological formations), geological and physiographical formations (including habitats of threatened species of animals and plants), and natural sites which are important from the point of view of science, conservation or natural beauty, are defined as natural heritage. The Slovak Republic ratified the convention on 31 March 1993, making its historical sites eligible for inclusion on the list. , there are eight World Heritage Sites in Slovakia. The first three sites in Slovakia were added to the list in 1993. These sites were Vlkolínec, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Show Caves In Slovakia
Show or The Show may refer to: Competition, event, or artistic production * Agricultural show, associated with agriculture and animal husbandry * Animal show, a judged event in the hobby of animal fancy ** Cat show ** Dog show ** Horse show ** Specialty show, a dog show which reviews a single breed *Show, an artistic production, such as: ** Concert ** Radio show ** Talk show ** Television show ** Theatre production * Trade fair or trade show Arts, entertainment, and media Films * ''The Show'' (1922 film), starring Oliver Hardy * ''The Show'' (1927 film), directed by Tod Browning * ''The Show'' (1995 film), a hip hop documentary * ''The Show'' (2017 film), an American satirical drama * ''The Show'' (2020 film), a British mystery film Album * ''Show'' (The Cure album), 1993 * ''Show'' (The Jesus Lizard album), 1994 * ''The Show'' (album), a 2008 album by eMC Songs * "The Show" (Doug E. Fresh song) * "The Show" (Girls Aloud song) * "The Show" (Lenka song) * "The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Caves In Slovakia
There are more than 2,400 caves in Slovakia, of which more than 400 have been explored so far. New caves are being discovered constantly. Caves open to the public * caves included in the UNESCO World Heritage Sites list: **Dobšiná Ice Cave (''Dobšinská ľadová jaskyňa''), Slovak Paradise **Domica, Slovak Karst **Gombasek Cave (''Gombasecká jaskyňa''), Slovak Karst ** Jasovská Cave (''Jasovská jaskyňa''), Slovak Karst **Ochtinská Aragonite Cave (''Ochtinská aragonitová jaskyňa''), Slovak Karst * other public caves: **Belianska Cave, Tatras ** Bojnická hradná jaskyňa (literally Bojnice Castle Cave), Bojnice ** Brestovská Cave (''Brestovská jaskyňa''), Western Tatras ** Bystrianska Cave (''Bystrianska jaskyňa''), Low Tatras **Cave of Dead Bats (''Jaskyňa mŕtvych netopierov''), Low Tatras **out of the Demänová Caves ( long), Low Tatras: *** Demänovská jaskyňa Slobody (literally Demänová Cave of Freedom) *** Demänovská Ice Cave (''Demänovská ľadová ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hron
The Hron ( sk, Hron; german: Gran; hu, Garam; la, Granus) is a long left tributary of the DanubePlán manažmentu povodňového rizikavčiastkovom povodí Hrona p. 38 and the second-longest river in . It flows from its source in the Low Tatra Mountains (below ) through central and southern Slovakia, emptying into the Danube near |
Bystra (river)
Bystra or Bystrá may refer to places: Czech Republic * Bystrá (Pelhřimov District) in the Vysočina Region * Bystrá nad Jizerou in the Liberec Region Poland * Bystra, Gorlice County in Lesser Poland Voivodeship (south Poland) * Bystra, Sucha County in Lesser Poland Voivodeship (south Poland) *Bystra, Bielsko County in Silesian Voivodeship (south Poland) *Bystra, Żywiec County in Silesian Voivodeship (south Poland) * Bystra, Pomeranian Voivodeship (north Poland) * Bystra, West Pomeranian Voivodeship (north-west Poland) Slovakia * Bystrá, Brezno District in the Banská Bystrica Region * Bystrá, Stropkov District in the Prešov Region *Bystrá (mountain) Bystrá is the highest mountain in the Western Tatras in Slovakia, near the Polish border. It is 2,248 meters high and surrounded by the valleys of Kamenistá, Račkova and Bystrá. See also *Tatra Mountains The Tatra Mountains (), Tatras, o ..., in the Western Tatras See also * Bystre (other) * Bystré (disam ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Speleotherapy
Speleotherapy (Greek σπήλαιον ''spḗlaion'' "cave") is an alternative medicine respiratory therapy involving breathing inside a cave. History Some sources claim that Hippocrates believed that salt-based therapies, including inhaling steam from saltwater, provided relief of respiratory symptoms. There are claims of improvements in the breathing of miners in Roman times and medieval times. Speleotherapy hospitals existed in Italy in the 19th century. In the middle of the 19th century, a clinic, founded in Mammoth Cave (Kentucky, USA), was intended for tuberculosis patients. However, a few months after the death of five of the patients, the hospital was closed. The history of modern speleotherapy dates back to the 1950s. At this time, speleotherapeutic hospitals arose in several Eastern and Central European countries. Residents of Ennepetal in Germany used the Kluterthöhle cave as a bomb shelter during WW2. Karl Hermann Spannagel began researching the therapeutic effect ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Speleotherapy
Speleotherapy (Greek σπήλαιον ''spḗlaion'' "cave") is an alternative medicine respiratory therapy involving breathing inside a cave. History Some sources claim that Hippocrates believed that salt-based therapies, including inhaling steam from saltwater, provided relief of respiratory symptoms. There are claims of improvements in the breathing of miners in Roman times and medieval times. Speleotherapy hospitals existed in Italy in the 19th century. In the middle of the 19th century, a clinic, founded in Mammoth Cave (Kentucky, USA), was intended for tuberculosis patients. However, a few months after the death of five of the patients, the hospital was closed. The history of modern speleotherapy dates back to the 1950s. At this time, speleotherapeutic hospitals arose in several Eastern and Central European countries. Residents of Ennepetal in Germany used the Kluterthöhle cave as a bomb shelter during WW2. Karl Hermann Spannagel began researching the therapeutic effect ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Precipice
In geography and geology, a cliff is an area of rock which has a general angle defined by the vertical, or nearly vertical. Cliffs are formed by the processes of weathering and erosion, with the effect of gravity. Cliffs are common on coasts, in mountainous areas, escarpments and along rivers. Cliffs are usually composed of rock that is resistant to weathering and erosion. The sedimentary rocks that are most likely to form cliffs include sandstone, limestone, chalk, and dolomite. Igneous rocks such as granite and basalt also often form cliffs. An escarpment (or scarp) is a type of cliff formed by the movement of a geologic fault, a landslide, or sometimes by rock slides or falling rocks which change the differential erosion of the rock layers. Most cliffs have some form of scree slope at their base. In arid areas or under high cliffs, they are generally exposed jumbles of fallen rock. In areas of higher moisture, a soil slope may obscure the talus. Many cliffs also featur ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
