Pokljuka
The Pokljuka Plateau () is a forested karst plateau at an elevation of around , located in the Julian Alps in northwestern Slovenia. The plateau is known for its forests, pasture, mountain pastures (Javornik, Lipanca, Uskovnica, Zajamniki, etc.), and winter sports facilities. It is also a common starting point for mountain hiking, hikers. The yearly Biathlon World Cup meets are held at the Pokljuka Biathlon Center, west of the town of Bled ( by car). Pokljuka is part of Triglav National Park. Administratively, it belongs to the Municipalities of Slovenia, municipalities of Municipality of Bled, Bled, Municipality of Bohinj, Bohinj, and Municipality of Gorje, Gorje. Many beech and fir trees were chopped down in the 18th century for the Iron foundry, iron foundries in Bohinj. They have been naturally replaced mostly by spruce trees. Some swamps can also be found, which is not usual on such high plateaus. Geography and geology Pokljuka is built of thick Upper Triassic limeston ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Bohinj
Bohinj (; ), or the Bohinj Valley () or Bohinj Basin (), is a 20 km long and 5 km wide basin in the Julian Alps, in the Upper Carniola region of northwestern Slovenia. It is traversed by the Sava Bohinjka river. Its main feature is the periglacial Lake Bohinj (). Bohinj is part of the Municipality of Bohinj, the seat of which is Bohinjska Bistrica. Geography The basin consists of four geographic units: the Lower Valley (), Upper Valley (), Ukanc Basin or Lake Basin (; Jezerska kotlina), and Nomenj Basin (). It is bounded by the Komarča head wall on one end and Soteska Canyon at the other. The Lower Bohinj Mountain Range represents its southern border. The Sava River has carved a canyon between the Jelovica and Pokljuka plateaus in the east. To the north, Mount Triglav, Slovenia's highest mountain, is also a part of the municipality. The Sava Bohinjka (which merges with the Sava Dolinka into the Sava) begins when two rivers, the Jezernica and the Mostnica, merge. The Mo ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Gorjuše
Gorjuše () is a high-elevation settlement on the Pokljuka Plateau in the Municipality of Bohinj in the Upper Carniola region of Slovenia Slovenia, officially the Republic of Slovenia, is a country in Central Europe. It borders Italy to the west, Austria to the north, Hungary to the northeast, Croatia to the south and southeast, and a short (46.6 km) coastline within the Adriati .... It is made up of the three disconnected hamlets of Spodnje Gorjuše, Srednje Gorjuše, and Zgornje Gorjuše (literally, 'lower, middle, and upper Gorjuše'). References External links *Gorjuše on Geopedia Populated places in the Municipality of Bohinj {{Bohinj-geo-stub ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Koprivnik V Bohinju
Koprivnik v Bohinju () is a settlement on the Pokljuka Plateau in the Municipality of Bohinj in the Upper Carniola region of Slovenia. Name The name of the settlement was changed from ''Koprivnik'' to ''Koprivnik v Bohinju'' (literally, 'Koprivnik in Bohinj') in 1955 to distinguish it from other settlements with the same name in Slovenia.''Spremembe naselij 1948–95''. 1996. Database. Ljubljana: Geografski inštitut ZRC SAZU, DZS. Church The local church is dedicated to the Exaltation of the Holy Cross The Feast of the Holy Cross, or Feast of the Cross, commemorates the cross used in the crucifixion of Jesus. In the Christian liturgical calendar, there are several different celebrations which honor and celebrate the cross used in the crucifi .... References External links *Koprivnik on Geopedia Populated places in the Municipality of Bohinj {{Bohinj-geo-stub ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Julian Alps
The Julian Alps (, , , , ) are a mountain range of the Southern Limestone Alps that stretches from northeastern Italy to Slovenia, where they rise to 2,864 m at Mount Triglav, the highest peak in Slovenia. A large part of the Julian Alps is included in Triglav National Park. The second highest peak of the range, the 2,755 m high Jôf di Montasio, lies in Italy. The Julian Alps cover an estimated 4,400 km2 (of which 1,542 km2 lies in Italy). They are located between the Sava Valley and Canale Valley. They are divided into the Eastern and Western Julian Alps. Name The Julian Alps were known in antiquity as ''Alpes Iuliae'', and also attested as ''Alpes Julianae'' AD 670, ''Alpis Julia'' 734, and ''Alpes Iulias'' in 1090. Like the municipium of ''Forum Julii'' (now Cividale del Friuli) at the foot of the mountains, the range was named after Julius Caesar of the gens Julia, perhaps due to a road built by Julius Caesar and completed by Augustus. Eastern Julian A ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Bled
Bled (; ,''Leksikon občin kraljestev in dežel zastopanih v državnem zboru,'' vol. 6: ''Kranjsko''. 1906. Vienna: C. Kr. Dvorna in Državna Tiskarna, p. 146. in older sources also ''Feldes'') is a town on Lake Bled in the Upper Carniolan region of northwestern Slovenia. It is one of Slovenia, Slovenia's most visited Resort town, tourist destinations. The town is the administrative seat of the Municipality of Bled. Name The town was first attested in written sources as ''Ueldes'' in 1004 (and as ''Veldes'' in 1011). The etymology of the name is unknown and it is believed to be of pre-Slavic origin. The German name of the town, ''Veldes'', was either borrowed from Old Slovene ''*Beldъ'' before AD 800 or is derived from the same pre-Slavic source as the Slovene name. Geography Bled is located on the southern foot of the Karawanks mountain range near the border with Austria, about northwest of the national capital of Ljubljana. South of Lake Bled are the densely forested Poklju ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Biathlon World Cup
The Biathlon World Cup is a top-level biathlon season-long competition series. It has been held since the winter seasons of 1977–78 for men and 1982–83 for women. The women's seasons until 1986–87 season were called the European Cup, although participation was not restricted to Europeans. Competition and format The World Cup season lasts from November or December to late March, with meetings in a different venue every week excluding some holidays and a couple of weeks before the season's major championships (World Championships or Winter Olympics). All in all, the season comprises nine to ten meetings, with events taking place from Wednesday–Thursday through Sunday. Relay competitions are held four to six times per season. Formerly it was counted as World Cup events are World Championships(the last Championship to count towards the World Cup were held in Pokljuka, Slovenia 2021) and Winter Olympics events (the last Olympics to count towards the World Cup were the 2010 ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Karst
Karst () is a topography formed from the dissolution of soluble carbonate rocks such as limestone and Dolomite (rock), dolomite. It is characterized by features like poljes above and drainage systems with sinkholes and caves underground. There is some evidence that karst may occur in more weathering-resistant rocks such as quartzite given the right conditions. Subterranean drainage may limit surface water, with few to no rivers or lakes. 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 Oil and gas reserves and resource quantification, hydrocarbon reserves are hosted in carbonate rock, and much of this is found in porous karst systems. Etymology ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Upper Triassic
The Late Triassic is the third and final epoch of the Triassic Period in the geologic time scale, spanning the time between Ma and Ma (million years ago). It is preceded by the Middle Triassic Epoch and followed by the Early Jurassic Epoch. The corresponding series of rock beds is known as the Upper Triassic. The Late Triassic is divided into the Carnian, Norian and Rhaetian ages. Many of the first dinosaurs evolved during the Late Triassic, including '' Plateosaurus'', ''Coelophysis'', '' Herrerasaurus'', and '' Eoraptor''. The Triassic–Jurassic extinction event began during this epoch and is one of the five major mass extinction events of the Earth. Etymology The Triassic was named in 1834 by Friedrich von Alberti, after a succession of three distinct rock layers (Greek meaning 'triad') that are widespread in southern Germany: the lower Buntsandstein (colourful sandstone'')'', the middle Muschelkalk (shell-bearing limestone) and the upper Keuper (coloured clay). The ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Swamps
A swamp is a forested wetland.Keddy, P.A. 2010. Wetland Ecology: Principles and Conservation (2nd edition). Cambridge University Press, Cambridge, UK. 497 p. Swamps are considered to be transition zones because both land and water play a role in creating this environment. Swamps vary in size and are located all around the world. The water of a swamp may be fresh water, brackish water, or seawater. Freshwater swamps form along large rivers or lakes where they are critically dependent upon rainwater and seasonal flooding to maintain natural water level fluctuations.Hughes, F.M.R. (ed.). 2003. The Flooded Forest: Guidance for policy makers and river managers in Europe on the restoration of floodplain forests. FLOBAR2, Department of Geography, University of Cambridge, Cambridge, UK. 96 p. Saltwater swamps are found along tropical and subtropical coastlines. Some swamps have hammock (ecology), hammocks, or dry-land protrusions, covered by aquatic vegetation, or vegetation that tolerate ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Groundwater
Groundwater is the water present beneath Earth's surface in rock and Pore space in soil, soil pore spaces and in the fractures of stratum, rock formations. About 30 percent of all readily available fresh water in the world is groundwater. A unit of rock or an unconsolidated deposit is called an ''aquifer'' when it can yield a usable quantity of water. The depth at which soil pore spaces or fractures and voids in rock become completely saturated with water is called the ''water table''. Groundwater is Groundwater recharge, recharged from the surface; it may discharge from the surface naturally at spring (hydrosphere), springs and Seep (hydrology), seeps, and can form oasis, oases or wetlands. Groundwater is also often withdrawn for agricultural, municipal, and industrial use by constructing and operating extraction water well, wells. The study of the distribution and movement of groundwater is ''hydrogeology'', also called groundwater hydrology. Typically, groundwater is thought o ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Dolomite (mineral)
Dolomite () is an anhydrous carbonate mineral composed of calcium magnesium carbonate, ideally The term is also used for a sedimentary carbonate rock composed mostly of the mineral dolomite (see Dolomite (rock)). An alternative name sometimes used for the dolomitic rock type is dolostone. History As stated by Nicolas-Théodore de Saussure the mineral dolomite was probably first described by Carl Linnaeus in 1768. In 1791, it was described as a rock by the French natural history, naturalist and geologist Déodat Gratet de Dolomieu (1750–1801), first in buildings of the old city of Rome, and later as samples collected in the County_of_Tyrol, Tyrolean Alps. Nicolas-Théodore de Saussure first named the mineral (after Dolomieu) in March 1792. Properties The mineral dolomite crystallizes in the trigonal, trigonal-rhombohedral system. It forms white, tan, gray, or pink crystals. Dolomite is a double carbonate, having an alternating structural arrangement of calcium and magnesium ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |