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Low Tatra
The Low Tatras or Low Tatra ( sk, Nízke Tatry; hu, Alacsony-Tátra) is a mountain range of the Inner Western Carpathians in central Slovakia. It is located south of the Tatras proper, from which it is separated by the valleys of the Váh and Poprad rivers (the Liptov-Spiš abasement). The valley formed by the Hron River is situated south of the Low Tatras range. The ridge runs west-eastwards and is about 80 km long. The Čertovica pass divides the range into two parts. The highest peaks of the Low Tatras are located in its western part. Ďumbier is the highest mountain at 2,042 m AMSL. Its neighbour Chopok (2,024 m) is accessible by a chairlift, and it is the most visited place in the Low Tatras. Other peaks in the western part include Dereše (2,004 m) and Chabenec (1,955 m). The highest peak in the eastern part is Kráľova hoľa (1,946 m). The best viewpoints in western part are Veľká Chochuľa, Salatín, Chabenec, Skalka, Chopok, Ďumbier, Siná, Poludnica a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Low Tatras - Blue Trail
Low or LOW or lows, may refer to: People * Low (surname), listing people surnamed Low Places * Low, Quebec, Canada * Low, Utah, United States * Lo Wu station (MTR code LOW), Hong Kong; a rail station * Salzburg Airport (ICAO airport code: LOWS), Austria Music * Low (band), an American indie rock group from Duluth, Minnesota Albums * Low (David Bowie album), ''Low'' (David Bowie album), 1977 * Low (Testament album), ''Low'' (Testament album), 1994 * Low (Low EP), ''Low'' (Low EP), 1994 Songs * Low (Cracker song), "Low" (Cracker song), 1993 * Low (Flo Rida song), "Low" (Flo Rida song), 2007 * Low (Foo Fighters song), "Low" (Foo Fighters song), 2002 * Low (Juicy J song), "Low" (Juicy J song), 2014 * Low (Kelly Clarkson song), "Low" (Kelly Clarkson song), 2003 * Low (Lenny Kravitz song), "Low" (Lenny Kravitz song), 2018 * Low (Sara Evans song), "Low" (Sara Evans song), 2008 * "Low", by Camp Mulla * "Low", by Coldplay from ''X&Y'' * "Low", by Inna from the Inna (album), self-titl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kráľova Hoľa
Kráľova hoľa (; german: link=no, Königsberg; hu, Király-hegy, literally "King's Bald Mountain") is the highest mountain (1,946 m) of the eastern part of the Low Tatras in central Slovakia. Four rivers rise at its foot: Čierny Váh, Hnilec, Hornád, and Hron. The summit, easily accessible by hiking trails from Telgárt as well as by a paved road from Šumiac (not open to motor vehicles, except for the mountain rescue service and maintenance workers of the TV transmitter on the summit), offers a panoramic view of Spiš, the Tatras, Liptov, and the Upper Hron Valley. Largely deforested by exploitative timber harvesting in the early 19th century, its timberline was restored to its natural elevation of about 1,650 m (5,413 ft.) through the efforts of Ludwig Greiner in the second half of that century. Kráľova hoľa is often depicted in Slovak folklore and Romantic poetry as a safe refuge of heroes and highwaymen, in particular Juraj Jánošík. As a metaphor of homelan ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tarn (lake)
A tarn (or corrie loch) is a Proglacial lake, proglacial mountain lake, pond or pool, formed in a cirque excavated by a glacier. A moraine may form a natural dam below a tarn. Etymology The word is toponymy, derived from the Old Norse word ''tjörn'' ("a small mountain lake without tributaries") meaning pond. In parts of Northern England - predominantly Cumbria but also areas of North Lancashire and North Yorkshire - 'tarn' is widely used as the name for small lakes or ponds, regardless of their location and origin (e.g. Talkin Tarn, Urswick Tarn, Malham Tarn). Similarly, in Scandinavian languages, a ''tjern'' or ''tjørn'' (both Norwegian) or ''tjärn'' or ''tärn'' (both Swedish) is a small natural lake, often in a forest or with vegetation closely surrounding it or growing into the tarn. The specific technical use for a body of water in a glacial corrie comes from high number of tarns found in corries in the Lake District, an upland area in Cumbria. Nonetheless, there are ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Važecká Cave
Važecká Cave ( sk, Važecká jaskyňa, and hu, Vázseci-barlang) is a long stalactite limestone cave. Lying at an elevation of , it is located near the village of Važec, in the Liptov Basin, near the Biely Váh River, on the northern edge of the Low Tatra mountain range in northern Slovakia Slovakia (; sk, Slovensko ), officially the Slovak Republic ( sk, Slovenská republika, links=no ), is a landlocked country in Central Europe. It is bordered by Poland to the north, Ukraine to the east, Hungary to the south, Austria to the s .... The cave was discovered in 1922. Of the 530 m total length, are open to the public. Although it is one of the shorter caves, it is known for its rich stalactite decoration, as well as for its cave fauna. External links Važecká Caveat Slovak Caves Administration Show caves in Slovakia Geography of Žilina Region Tourist attractions in Žilina Region {{Slovakia-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cave Of Dead Bats
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, microorganism ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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] |
Gneiss
Gneiss ( ) is a common and widely distributed type of metamorphic rock. It is formed by high-temperature and high-pressure metamorphic processes acting on formations composed of igneous or sedimentary rocks. Gneiss forms at higher temperatures and pressures than schist. Gneiss nearly always shows a banded texture characterized by alternating darker and lighter colored bands and without a distinct cleavage. Gneisses are common in the ancient crust of continental shields. Some of the oldest rocks on Earth are gneisses, such as the Acasta Gneiss. Description Orthogneiss from the Czech Republic In traditional English and North American usage, a gneiss is a coarse-grained metamorphic rock showing compositional banding (gneissic banding) but poorly developed schistosity and indistinct cleavage. In other words, it is a metamorphic rock composed of mineral grains easily seen with the unaided eye, which form obvious compositional layers, but which has only a weak tendency to fracture ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Granite
Granite () is a coarse-grained (phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or ''granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) contain almost no dark minerals. Granite is nearly alway ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Strata
In geology and related fields, a stratum ( : strata) is a layer of rock or sediment characterized by certain lithologic properties or attributes that distinguish it from adjacent layers from which it is separated by visible surfaces known as either '' bedding surfaces'' or ''bedding planes''.Salvador, A. ed., 1994. ''International stratigraphic guide: a guide to stratigraphic classification, terminology, and procedure. 2nd ed.'' Boulder, Colorado, The Geological Society of America, Inc., 215 pp. . Prior to the publication of the International Stratigraphic Guide, older publications have defined a stratum as either being either equivalent to a single bed or composed of a number of beds; as a layer greater than 1 cm in thickness and constituting a part of a bed; or a general term that includes both ''bed'' and ''lamina''.Neuendorf, K.K.E., Mehl, Jr., J.P., and Jackson, J.A. , eds., 2005. ''Glossary of Geology'' 5th ed. Alexandria, Virginia, American Geological Institute. 779 pp. . ... [...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] |
