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Slovak Karst
The Slovak Karst ( sk, Slovenský kras) is one of the mountain ranges of the Slovenské Rudohorie Mountains in the Carpathians in southern Slovakia. It consists of a complex of huge karst plains and plateaus. Since 1973 it has been a protected landscape area. On 1 March 2002 Slovak Karst National Park was declared. It is also a UNESCO Biosphere Reserve and part of it forms UNESCO World Heritage site Caves of Aggtelek Karst and Slovak Karst. Characteristics The highest peak is Jelení vrch at 947 m AMSL. Important rivers are the Slaná (Sajó), the Štítnik and the Turňa. The Slovak Karst lies in the north temperate zone and has a continental climate with four distinct seasons. The area is composed of several layers of Mesozoic limestone and dolomite, beneath which there is non-permeable sandstone, limestone and slate. The plains are covered by oak-hornbeam forests, the hills by oak forests and the karst pits by spruce forests. Beech forests are in the northern parts. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Slovenský Kras
The Slovak Karst ( sk, Slovenský kras) is one of the mountain ranges of the Slovenské Rudohorie Mountains in the Carpathians in southern Slovakia. It consists of a complex of huge karst plains and plateaus. Since 1973 it has been a protected landscape area. On 1 March 2002 Slovak Karst National Park was declared. It is also a UNESCO Biosphere Reserve and part of it forms UNESCO World Heritage site Caves of Aggtelek Karst and Slovak Karst. Characteristics The highest peak is Jelení vrch at 947 m AMSL. Important rivers are the Slaná (Sajó), the Štítnik and the Turňa. The Slovak Karst lies in the north temperate zone and has a continental climate with four distinct seasons. The area is composed of several layers of Mesozoic limestone and dolomite, beneath which there is non-permeable sandstone, limestone and slate. The plains are covered by oak-hornbeam forests, the hills by oak forests and the karst pits by spruce forests. Beech forests are in the northern parts. The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dolomite (rock)
Dolomite (also known as dolomite rock, dolostone or dolomitic rock) is a sedimentary carbonate rock that contains a high percentage of the mineral dolomite, CaMg(CO3)2. It occurs widely, often in association with limestone and evaporites, though it is less abundant than limestone and rare in Cenozoic rock beds (beds less than about 66 million years in age). The first geologist to distinguish dolomite rock from limestone was Belsazar Hacquet in 1778. Most dolomite was formed as a magnesium replacement of limestone or of lime mud before lithification. The geological process of conversion of calcite to dolomite is known as dolomitization and any intermediate product is known as dolomitic limestone. The "dolomite problem" refers to the vast worldwide depositions of dolomite in the past geologic record in contrast to the limited amounts of dolomite formed in modern times. Recent research has revealed sulfate-reducing bacteria living in anoxic conditions precipitate dolomite which ind ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Krásnohorská Cave
Krásnohorská Cave ( sk, Krásnohorská Jaskyňa) is a karst cave situated at the northern foot of the Silická planina Plain, in the Slovak Karst, 6.5 km southeast of Rožňava, in Slovakia. With unique natural decorations of bizarre shapes and unusual structure composed almost entirely of calcium, it is currently listed by the Guinness Book of Records as the cave containing the largest stalagmite in existence, generally accepted as being about in diameter and in height. It grows significantly in volume every year as the incessant drips solidify. The length of the cave is to and it represents the end of the cave system underground stream Buzgó. Description Part of the cave from the entrance to the Hall of Giants (''Sieň obrov'') is formed in dolomite and dolomitic limestones with impressive limestone layers. The back parts of the cave, like the Pearl Passage (''Chodba perál''), the Great Hall (''Veľká sieň''), and the Mirror Hall (''Zrkadlová sieň''), are loc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jasovská Cave
Jasov Cave ( sk, Jasovská jaskyňa, and hu, Jászói barlang) is a speleothem limestone cave and archaeological site in the Slovak Karst in Slovakia. It is located near the village of Jasov, around from Košice city. History The cave was partly opened for the public in 1846, making it the oldest publicly accessible cave in Slovakia. The lower parts of the cave were discovered in 1922 to 1924 and a concrete footpath was built and electrical lightning was installed in 1924. out of are open to the public. Many archaeological discoveries of the Paleolithic, Neolith and the Hallstatt periods have been made in the cave. Along with a number of caves of the Slovak Karst, Jasov Cave has been induced into the UNESCO World Heritage list as a part of the Caves of Aggtelek Karst and Slovak Karst The Caves of Aggtelek Karst and Slovak Karst is a UNESCO World Heritage site consisting of 712 caves spread out over a total area of along the border of Hungary and Slovakia. Background ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gombasek Cave
Gombasek Cave or Gombasecká jaskyňa (in Slovak language, Slovak) and Gombaszögi-barlang (in Hungarian language, Hungarian) is a karst cave in the Slovak Karst, Slovakia. It is named after the settlement of ''Gombasek'', which belongs to the village of Slavec. It is located in the Slovak Karst National Park, in the Slaná river valley, approximately 15 km south of Rožňava. The cave was discovered on 21 November 1951 by volunteer cavers. In 1955, 285 m out of 1 525 m were opened to the public. Currently, the route for visitors is 530 m long and takes about 30 minutes. The cave was also used for "speleotherapy" as a sanatorium, focused on airway diseases. Since 1995, the Gombasek Cave is included in the UNESCO World Heritage list as a part of Caves of Aggtelek Karst and Slovak Karst. See also *List of caves in Slovakia External linksGombasek CaveaSlovakia.travel [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ochtinská Aragonite Cave
Ochtinská Aragonite Cave ( sk, Ochtinská aragonitová jaskyňa, hu, Martonházi-aragonitbarlangthe Magyar Wikipedia article uses a different title) is a unique aragonite cave situated in southern Slovakia, near Rožňava. Although only 300 m long, it is famous for its rare aragonite formations. Description There are only three aragonite caves discovered in the world so far. In the so-called Milky Way Hall, the main attraction of the cave, white branches and clusters of aragonite shine like stars in the Milky Way. The cave was discovered by Martin Cangár and Jiri Prosek in 1954 and opened to the public in 1972. Along with other caves of the Slovak Karst, it is included in the UNESCO World Heritage list as a component of Caves of Aggtelek Karst and Slovak Karst site. See also *List of caves in Slovakia Gallery Image:Ochtina Aragonite Cave 28.jpg, Aragonite inside the cave References External links Official site with pictures, map of the cave, and contact information ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Domica
The Domica cave is situated on the south-western border of the ''Silicka planina Plateau'' south-east of Plesivec in the Rožňava District of the Košice Region in southern Slovakia and in combination with the Baradla cave represents the most significant section of the ''Aggtelek Karst and Slovak Karst'' cross-border cave network that continues into the ( Aggtelek National Park) in Hungary. These vast limestone passages, that had formed during the Middle Triassic and are rich in speleothems were discovered in 1926 by Ján Majko. A section of its total length of is publicly accessible since 1932. As an element of the ''Caves of Aggtelek Karst and Slovak Karst'' the site has been induced into the UNESCO World Heritage list in 1995. Exploration The site belongs to a complex variety of formations that include 712 caves, many of which were well known among the local population for centuries. Bartholomeides, a priest from Ochtiná documented his first systematic excursions into ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cave
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, microorgani ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Domica Cave 22
The Domica cave is situated on the south-western border of the ''Silicka planina Plateau'' south-east of Plesivec in the Rožňava District of the Košice Region in southern Slovakia and in combination with the Baradla cave represents the most significant section of the ''Aggtelek Karst and Slovak Karst'' cross-border cave network that continues into the ( Aggtelek National Park) in Hungary. These vast limestone passages, that had formed during the Middle Triassic and are rich in speleothems were discovered in 1926 by Ján Majko. A section of its total length of is publicly accessible since 1932. As an element of the ''Caves of Aggtelek Karst and Slovak Karst'' the site has been induced into the UNESCO World Heritage list in 1995. Exploration The site belongs to a complex variety of formations that include 712 caves, many of which were well known among the local population for centuries. Bartholomeides, a priest from Ochtiná documented his first systematic excursions into ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Beech
Beech (''Fagus'') is a genus of deciduous trees in the family Fagaceae, native to temperate Europe, Asia, and North America. Recent classifications recognize 10 to 13 species in two distinct subgenera, ''Engleriana'' and ''Fagus''. The ''Engleriana'' subgenus is found only in East Asia, distinctive for its low branches, often made up of several major trunks with yellowish bark. The better known ''Fagus'' subgenus beeches are high-branching with tall, stout trunks and smooth silver-grey bark. The European beech (''Fagus sylvatica'') is the most commonly cultivated. Beeches are monoecious, bearing both male and female flowers on the same plant. The small flowers are unisexual, the female flowers borne in pairs, the male flowers wind-pollinating catkins. They are produced in spring shortly after the new leaves appear. The fruit of the beech tree, known as beechnuts or mast, is found in small burrs that drop from the tree in autumn. They are small, roughly triangular, and edible, w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Spruce
A spruce is a tree of the genus ''Picea'' (), a genus of about 35 species of coniferous evergreen trees in the family Pinaceae, found in the northern temperate and boreal (taiga) regions of the Earth. ''Picea'' is the sole genus in the subfamily Piceoideae. Spruces are large trees, from about 20 to 60 m (about 60–200 ft) tall when mature, and have whorled branches and conical form. They can be distinguished from other members of the pine family by their needles (leaves), which are four-sided and attached singly to small persistent peg-like structures (pulvini or sterigmata) on the branches, and by their cones (without any protruding bracts), which hang downwards after they are pollinated. The needles are shed when 4–10 years old, leaving the branches rough with the retained pegs. In other similar genera, the branches are fairly smooth. Spruce are used as food plants by the larvae of some Lepidoptera (moth and butterfly) species, such as the eastern spruce budwo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
