Skuta Glacier
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Skuta Glacier
Skuta Glacier (Slovenian: ''Ledenik pod Skuto''), located beneath mountain Skuta in Kamnik-Savinja Alps in Slovenia is the most south-eastern glacier in the Alps. Geography Skuta Glacier had an area of in 1950 and in 2013. Reaching above sea level at its lowest point, it is also one of the lowest elevation glaciers in the Alps. Triglav Triglav (; german: Terglau; it, Tricorno), with an elevation of , is the highest mountain in Slovenia and the highest peak of the Julian Alps. The mountain is the pre-eminent symbol of the Slovene nation. It is the centrepiece of Triglav Natio ... glacieret is the second remaining glacier in Slovenia at the elevation of 2500 m. Skuta Glacier in figures * Area: (as of 2007) * Elevation: * Average ice thickness: (as of September 2006) * Maximum ice thickness: (as of September 2006) * Volume: (as of September 2006) Skuta Glacier.JPG, Snow fields beneath the glacier File:Snow fields benetah Skuta Glacier, Slovenia.1.jpg, Snow fi ...
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Skuta
Skuta (, ) is the third-highest peak in the Kamnik Alps and is known for the Skuta Glacier, which is the easternmost glacier in the Alps. A mountain lodge, operated by the Ljubljana Matica Alpine Club, stands below Skuta. Name Although the Slovene common noun ''skuta'' refers to a ricotta Ricotta ( in Italian) is an Italian whey cheese made from sheep, cow, goat, or Italian water buffalo milk whey left over from the production of other cheeses. Like other whey cheeses, it is made by coagulating the proteins that remain after the ...-like cheese, there is no evidence that this word is the source of the mountain's name. References External links Skuta on hribi.net Route Description and Photos (slo)Skuta on SummitPost.org Mountains of the Kamnik–Savinja Alps Mountains of Upper Carniola Two-thousanders of Slovenia {{Slovenia-geo-stub ...
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Slovene Language
Slovene ( or ), or alternatively Slovenian (; or ), is a South Slavic languages, South Slavic language, a sub-branch that is part of the Balto-Slavic languages, Balto-Slavic branch of the Indo-European languages, Indo-European language family. It is spoken by about 2.5 million speakers worldwide (excluding speakers of Kajkavian), mainly ethnic Slovenes, the majority of whom live in Slovenia, where it is the sole official language. As Slovenia is part of the European Union, Slovene is also one of its 24 Languages of the European Union, official and working languages. Standard Slovene Standard Slovene is the national standard language that was formed in the 18th and 19th century, based on Upper Carniolan dialect group, Upper and Lower Carniolan dialect groups, more specifically on language of Ljubljana and its adjacent areas. The Lower Carniolan dialect group was the dialect used in the 16th century by Primož Trubar for his writings, while he also used Slovene as spoken in Lju ...
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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 ...
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Alps
The Alps () ; german: Alpen ; it, Alpi ; rm, Alps ; sl, Alpe . are the highest and most extensive mountain range system that lies entirely in Europe, stretching approximately across seven Alpine countries (from west to east): France, Switzerland, Italy, Liechtenstein, Austria, Germany, and Slovenia. The Alpine arch generally extends from Nice on the western Mediterranean to Trieste on the Adriatic and Vienna at the beginning of the Pannonian Basin. The mountains were formed over tens of millions of years as the African and Eurasian tectonic plates collided. Extreme shortening caused by the event resulted in marine sedimentary rocks rising by thrusting and folding into high mountain peaks such as Mont Blanc and the Matterhorn. Mont Blanc spans the French–Italian border, and at is the highest mountain in the Alps. The Alpine region area contains 128 peaks higher than . The altitude and size of the range affect the climate in Europe; in the mountains, precipitation ...
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Triglav
Triglav (; german: Terglau; it, Tricorno), with an elevation of , is the highest mountain in Slovenia and the highest peak of the Julian Alps. The mountain is the pre-eminent symbol of the Slovene nation. It is the centrepiece of Triglav National Park, Slovenia's only national park. Triglav was also the highest peak in Yugoslavia before Slovenia's independence in 1991. Name Various names have been used for the mountain through history. An old map from 1567 named it ''Ocra mons'', whereas Johann Weikhard von Valvasor named it ''Krma'' in the second half of the 17th century. According to the German mountaineer and professor Adolf Gstirner, the name ''Triglav'' first appeared in written sources as ''Terglau'' in 1452, but the original source has been lost. The next known occurrence of ''Terglau'' is cited by Gstirner and is from a court description of the border in 1573. Early forms of the name ''Triglav'' also include ''Terglau'' in 1612, ''Terglou'' in 1664 and ''Terklou'' arou ...
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Glaciers Of Slovenia
A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its ablation over many years, often centuries. It acquires distinguishing features, such as crevasses and seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on every continent other than the Australian mainland, including Oceania's high-latitude oceanic island countries such as New Zealand. Between latitudes 35°N and 35°S, glaciers occur ...
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Glaciers Of The Alps
A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its ablation over many years, often centuries. It acquires distinguishing features, such as crevasses and seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on every continent other than the Australian mainland, including Oceania's high-latitude oceanic island countries such as New Zealand. Between latitudes 35°N and 35°S, glaciers occur only in ...
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