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Belianske Tatras
, photo = Belianske Tatry from Jahňaci štít-captions sk.svg , photo_size = 250px , photo_caption = Muráň, Nový, Havran, Ždiarska Vidla peaks – beginning from the left , country = Slovakia , region = Prešov , region_type = Region , district = Poprad , parent = Eastern Tatras , border = , border1 = , geology = , geology1 = , period = , period1 = , orogeny = , area_km2 = , length_km = , length_orientation = , width_km = , width_orientation = , highest = , highest_location = , elevation_m = 2151.5 , range_coordinates = , ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Muráň (mountain)
Muráň (earlier ''Podmuráň'', german: Untermuran, hu, Murányalja) is a village and municipality in Revúca District in the Banská Bystrica Region of Slovakia. Geography The village is located around 9 km north of Revúca, in the Muráň river valley. The Muráň Plateau is located north and west of the village, with the governing body of the Muránska planina National Park seated in the village. There is a local railway track from Plešivec (Rožňava District) ending in Muráň. History The village was first mentioned in 1321 as a settlement under the Muráň Castle. King Ferdinand I of Bulgaria , image = Zar Ferdinand Bulgarien.jpg , caption = Ferdinand in 1912 , reign = 5 October 1908 – , coronation = , succession = Tsar of Bulgaria , predecessor = Himself as Prince , successor = Boris III , rei ... had a manor house in the village, Predná Hora mansion, which is now a specialized hospital. References External lin ... [...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] |
Mountain Ranges Of The Western Carpathians
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain Ranges Of Slovakia
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Edelweiss
EDELWEISS (Expérience pour DEtecter Les WIMPs En Site Souterrain) is a dark matter search experiment located at the Modane Underground Laboratory in France. The experiment uses cryogenic detectors, measuring both the phonon and ionization signals produced by particle interactions in germanium crystals. This technique allows nuclear recoils events to be distinguished from electron recoil events. The EURECA project is a proposed future dark matter experiment, which will involve researchers from EDELWEISS and the CRESST dark matter search. Dark matter Dark matter is material which does not emit or absorb light. Measurements of the rotation curves of spiral galaxies suggest it makes up the majority of the mass of galaxies; and precision measurements of the cosmic microwave background radiation suggest it accounts for a significant fraction of the density of the Universe. A possible explanation of dark matter comes from particle physics. WIMP (Weakly Interacting Massive Particl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Endemism
Endemism is the state of a species being found in a single defined geographic location, such as an island, state, nation, country or other defined zone; organisms that are indigenous to a place are not endemic to it if they are also found elsewhere. For example, the Cape sugarbird is found exclusively in southwestern South Africa and is therefore said to be ''endemic'' to that particular part of the world. An endemic species can be also be referred to as an ''endemism'' or in scientific literature as an ''endemite''. For example '' Cytisus aeolicus'' is an endemite of the Italian flora. '' Adzharia renschi'' was once believed to be an endemite of the Caucasus, but it was later discovered to be a non-indigenous species from South America belonging to a different genus. The extreme opposite of an endemic species is one with a cosmopolitan distribution, having a global or widespread range. A rare alternative term for a species that is endemic is "precinctive", which applies to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tatra Chamois
The Tatra chamois (''Rupicapra rupicapra tatrica''; sk, Kamzík vrchovský tatranský; pl, Kozica tatrzańska) is a subspecies of the chamois of the genus '' Rupicapra''. Tatra chamois live in the Tatra Mountains in Slovakia and Poland. Population and distribution The Tatra chamois live in all parts of the Tatras: West Tatras (Slovakia and Poland) and Eastern Tatras, which consist of the High Tatras (Slovakia and Poland) and the Belianske Tatras (Slovakia), all protected by national parks in both countries. The population has undergone several troughs and peaks in known history, with the most noticeable troughs occurring during both world wars. The largest population in the 20th century was recorded in the year 1964, when as much as 940 individuals were counted in the Slovak region of the Tatras. Subsequently, the population declined steadily to the lowest recorded numbers in history at the end of the century. During the years 1999-2000 numbers dropped below 200 individuals ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tatra National Park, Slovakia
Tatra(s) National Park ( sk, Tatranský národný park; abbr. TANAP) is one of the nine national parks in Slovakia. It is situated in North Central Slovakia in the Tatra Mountains. The park is important for protecting a diverse variety of flora and fauna, with many endemic species, including the Tatra chamois. The Tatra Mountains form a natural border between Slovakia to the north and Poland to the south, and the two countries have cooperated since the early 20th century on efforts to protect the area. Poland created an adjoining national park, and UNESCO later designated the combined effort a transboundary biosphere reserve. Geography The Tatra National Park protects the Slovak areas of the High Tatras mountain range in the Eastern Tatras (''Východné Tatry'') ranges, and areas of the Western Tatras (''Západné Tatry'') ranges. The west part of the Tatra National Park is situated in the Žilina Region and the east part in the Prešov Region. The national park covers an a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Belianska Cave
Belianska Cave ( sk, Belianska jaskyňa, ) is a stalactite cave in the Slovak part of the Tatra mountains The Tatra Mountains (), Tatras, or Tatra (''Tatry'' either in Slovak () or in Polish () - '' plurale tantum''), are a series of mountains within the Western Carpathians that form a natural border between Slovakia and Poland. They are the hi ..., the largest and the only one open to the public in the Tatras. It is located above the settlement of Tatranská Kotlina, which is a part of the town of Vysoké Tatry. The cave was discovered in the 18th century, although it is presumed that it was used by pre-historic people. The cave was opened in 1884 and electrically lit in 1896. Entrance to the cave is located at an altitude of 890 metres. The cave is 3,641 m long, with two circuits available to the visitors, with the longer one having the length of 1,752 m. References External links Belianska Cave at the Slovak Caves AdministrationBelianska CaveaSlovakia.travel ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...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] |
Shepherds
A shepherd or sheepherder is a person who tends, herds, feeds, or guards flocks of sheep. ''Shepherd'' derives from Old English ''sceaphierde (''sceap'' 'sheep' + ''hierde'' 'herder'). ''Shepherding is one of the world's oldest occupations, it exists in all parts of the globe, and it is an important part of pastoralist animal husbandry. Because of the ubiquity of the profession, many religions and cultures have symbolic or metaphorical references to the shepherd profession. For example, Jesus called himself the Good Shepherd, and ancient Greek mythologies highlighted shepherds such as Endymion and Daphnis. This symbolism and shepherds as characters are at the center of pastoral literature and art. Origins Shepherding is among the oldest occupations, beginning some 5,000 years ago in Asia Minor. Sheep were kept for their milk, meat and especially their wool. Over the next thousand years, sheep and shepherding spread throughout Eurasia. Henri Fleisch tentatively suggested ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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