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Komna
Komna is a mountain karst plateau in the Julian Alps in northwestern Slovenia. It has an elevation from to . It has a triangular shape and rises above the Bohinj Basin. To the east, it continues into the Triglav Lakes Valley. The lowest measured temperatures in Slovenia were recorded at Komna in January 2009, reaching . The Komna Lodge is situated on Komna at an elevation of . It is operated by the Ljubljana Matica Alpine Club The Ljubljana Matica Alpine Club ( sl, Planinsko društvo Ljubljana-Matica, shortly or simply ), with its office located in Ljubljana, is by the number of members the largest Alpine club in Slovenia. In 2013, the club had about 2,800 members. It i .... References External links * {{coord, 46, 17, 4.06, N, 13, 46, 24.17, E, type:mountain_region:SI_dim:5800, display=title Karst plateaus of Slovenia Julian Alps Plateaus in Upper Carniola ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Komna Lodge
Komna is a mountain karst plateau in the Julian Alps in northwestern Slovenia. It has an elevation from to . It has a triangular shape and rises above the Bohinj Basin. To the east, it continues into the Triglav Lakes Valley. The lowest measured temperatures in Slovenia were recorded at Komna in January 2009, reaching . The Komna Lodge is situated on Komna at an elevation of . It is operated by the Ljubljana Matica Alpine Club The Ljubljana Matica Alpine Club ( sl, Planinsko društvo Ljubljana-Matica, shortly or simply ), with its office located in Ljubljana, is by the number of members the largest Alpine club in Slovenia. In 2013, the club had about 2,800 members. It i .... References External links * {{coord, 46, 17, 4.06, N, 13, 46, 24.17, E, type:mountain_region:SI_dim:5800, display=title Karst plateaus of Slovenia Julian Alps Plateaus in Upper Carniola ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Triglav Lakes Valley
The Triglav Lakes Valley ( sl, Dolina Triglavskih jezer) is a rocky hanging valley in the Julian Alps in Slovenia, below the sheer sides of Mount Tičarica and Mount Zelnarica southwest of Triglav. The valley is also called the Seven Lakes Valley (), although there are ten and not seven lakes in the valley. It is above the tree line and is geologically alpine karst; therefore it has also been termed the Sea of Stone Valley (). Lakes The lowest lake is the Black Lake () at an elevation of above sea level; it is above the rocky slope of the Komarča Crag. The Alpine newt (''Ichthyosaura alpestris''), endemic to the Alps, lives in it. Below Mount Tičarica (elevation ) there are two interconnected lakes known as the Double Lake (). At an elevation of lies the Big Lake () or the Lake Ledvica (literally: Lake Kidney; ). It has the shape of a kidney and is the largest and the deepest of these lakes. The highest is the Podstenje Lake (), which is located at an elevation of . Mou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ljubljana Matica Alpine Club
The Ljubljana Matica Alpine Club ( sl, Planinsko društvo Ljubljana-Matica, shortly or simply ), with its office located in Ljubljana, is by the number of members the largest Alpine club in Slovenia. In 2013, the club had about 2,800 members. It is a member of the Alpine Association of Slovenia. The current president of the club is Tomaž Willenpart. Sections of the club are involved in hillwalking, mountaineering, mountain biking, hike guiding and mountain guiding, mountain rescue, maintenance of trails, youth education, publishing and the conservation of the mountain environment. The club operates the following mountain shelters: the Triglav Lodge at Kredarica, the Triglav Lakes Lodge, the Savica Lodge, the Kamnik Bistrica Lodge, the Komna Lodge, and the Mali Podi Shelter below Mt. Skuta. The year of establishment of the club is disputed. According to the club, it was established in 1893 along with the Slovene Alpine Club (; SPD), under the name Central SPD Club (), and ... [...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] |
Plateau
In geology and physical geography, a plateau (; ; ), also called a high plain or a tableland, is an area of a highland consisting of flat terrain that is raised sharply above the surrounding area on at least one side. Often one or more sides have deep hills or escarpments. Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, and erosion by water and glaciers. Plateaus are classified according to their surrounding environment as intermontane, piedmont, or continental. A few plateaus may have a small flat top while others have wide ones. Formation Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, Plate tectonics movements and erosion by water and glaciers. Volcanic Volcanic plateaus are produced by volcanic activity. The Columbia Plateau in the north-western United States is an example. They may be formed by upwelling of volcanic magma or extrusion of lava. The un ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Julian Alps
The Julian Alps ( sl, Julijske Alpe, it, Alpi Giulie, , ) are a mountain range of the Southern Limestone Alps that stretch 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 ''Alpe Iulia'', and also attested as ''Alpes Juliana'' 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 Julian clan, perhaps due to a road built by Julius Caesar and completed by Aug ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Slovenia
Slovenia ( ; sl, Slovenija ), officially the Republic of Slovenia (Slovene: , abbr.: ''RS''), is a country in Central Europe. It is bordered by Italy to the west, Austria to the north, Hungary to the northeast, Croatia to the southeast, and the Adriatic Sea to the southwest. Slovenia is mostly mountainous and forested, covers , and has a population of 2.1 million (2,108,708 people). Slovenes constitute over 80% of the country's population. Slovene, a South Slavic language, is the official language. Slovenia has a predominantly temperate continental climate, with the exception of the Slovene Littoral and the Julian Alps. A sub-mediterranean climate reaches to the northern extensions of the Dinaric Alps that traverse the country in a northwest–southeast direction. The Julian Alps in the northwest have an alpine climate. Toward the northeastern Pannonian Basin, a continental climate is more pronounced. Ljubljana, the capital and largest city of Slovenia, is geogr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bohinj
Bohinj (; german: Wochein), or the Bohinj Valley ( sl, Bohinjska dolina) or Bohinj Basin ( sl, Bohinjska kotlina), 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 ( sl, Bohinjsko jezero). 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 ( sl, Spodnja dolina), 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 th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Karst Plateaus Of Slovenia
Karst is a topography formed from the dissolution of soluble rocks such as limestone, Dolomite (rock), 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 language, German in the late 19th century, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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