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Mangart Saddle
Mangart Saddle or the Mangart Pass ( sl, Mangartsko sedlo or ) is a mountain saddle in the Julian Alps in northwestern Slovenia. It has an elevation of . It is the most common starting point for the ascent of Mt. Mangart (). The Mangart Road () that leads over Mangart Saddle, with its elevation of , has a number of turns and is the highest-lying road in Slovenia. It was built in 1938. The Mangart Pass offers a picturesque view towards the Log Koritnica Valley in Slovenia to the south and the Lakes of Fusine in Italy to the north. The Mangart Saddle Lodge () lies under the saddle. The saddle was the scenery of the film ''Let's Go Our Own Way''. Mangart Saddle is also known as the finding place of manganese nodules from the Early Jurassic The Early Jurassic Epoch (geology), Epoch (in chronostratigraphy corresponding to the Lower Jurassic series (stratigraphy), Series) is the earliest of three epochs of the Jurassic Period. The Early Jurassic starts immediately after the Triassic-J ...
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Mangart 14
Mangart or Mangrt is a mountain in the Julian Alps, located on the border between Italy and Slovenia. With an elevation of , it is the third-highest peak in Slovenia, after Triglav and Škrlatica. It was first climbed in 1794 by the naturalist Franz von Hohenwart. Mangart is also the name of the mountain range between the Koritnica Valley and the Mangart Valley, with the highest peak called ''Veliki Mangart'' (Big Mount Mangart). Name Mount Mangart was attested in historical sources in 1617 as ''Monhart''. The name is of German origin, derived from the personal name ''Mainhart'' (from Old High German ''Maganhard''). In addition to serving as the name of the mountain, this German name has also developed into Slovene surnames such as ''Manhart'' and ''Menart''. Access The road to Mangart Saddle Mangart Saddle or the Mangart Pass ( sl, Mangartsko sedlo or ) is a mountain saddle in the Julian Alps in northwestern Slovenia. It has an elevation of . It is the most common starting poi ...
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Mountain Saddle
In geomorphology, a col is the lowest point on a mountain ridge between two peaks.Whittow, John (1984). ''Dictionary of Physical Geography''. London: Penguin, 1984, p. 103. . It may also be called a gap. Particularly rugged and forbidding cols in the terrain are usually referred to as notches. They are generally unsuitable as mountain passes, but are occasionally crossed by mule tracks or climbers' routes. The term col tends to be associated more with mountain rather than hill ranges. It is derived from the French ''col'' ("collar, neck") from Latin ''collum'', "neck". The height of a summit above its highest col (called the key col) is effectively a measure of a mountain's topographic prominence. Cols lie on the line of the watershed between two mountains, often on a prominent ridge or arête. For example, the highest col in Austria, the ''Obere Glocknerscharte'' ("Upper Glockner Col", ), lies between the Kleinglockner () and Grossglockner () mountains, giving the Kleinglockn ...
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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 ...
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Mangart
Mangart or Mangrt is a mountain in the Julian Alps, located on the border between Italy and Slovenia. With an elevation of , it is the third-highest peak in Slovenia, after Triglav and Škrlatica. It was first climbed in 1794 by the naturalist Franz von Hohenwart. Mangart is also the name of the mountain range between the Koritnica Valley and the Mangart Valley, with the highest peak called ''Veliki Mangart'' (Big Mount Mangart). Name Mount Mangart was attested in historical sources in 1617 as ''Monhart''. The name is of German origin, derived from the personal name ''Mainhart'' (from Old High German ''Maganhard''). In addition to serving as the name of the mountain, this German name has also developed into Slovene surnames such as ''Manhart'' and ''Menart''. Access The road to Mangart Saddle Mangart Saddle or the Mangart Pass ( sl, Mangartsko sedlo or ) is a mountain saddle in the Julian Alps in northwestern Slovenia. It has an elevation of . It is the most common starting po ...
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Log Koritnica Valley
Log most often refers to: * Trunk (botany), the stem and main wooden axis of a tree, called logs when cut ** Logging, cutting down trees for logs ** Firewood, logs used for fuel ** Lumber or timber, converted from wood logs * Logarithm, in mathematics Log, LOG or LoG may also refer to: Arts, entertainment and media * ''Log'' (magazine), an architectural magazine * ''The Log'', a boating and fishing newspaper published by the Duncan McIntosh Company * Lamb of God (band) or LoG, an American metal band * The Log, an electric guitar by Les Paul * Log, a fictional product in ''The Ren & Stimpy Show'' * The League of Gentlemen or LoG, a British comedy show. Places * Log, Russia, the name of several places * Log, Slovenia, the name of several places Science and mathematics *Logarithm, a mathematical function * Log file, a computer file in which events are recorded * Laplacian of Gaussian or LoG, an algorithm used in digital image processing Other uses * Logbook, or log, a record ...
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Lakes Of Fusine
Fusine in Valromana ( sl, Fužine or ; german: Weißenfels; Friulian: ''Fusinis'') is a ''frazione'' (fractional parish) of the ''comune'' of Tarvisio in the Province of Udine, in the autonomous Friuli-Venezia Giulia region of northeastern Italy. Name The locality takes its name from the Slovene (''Fužine'') and Friulian (''Fusinis'') term for the historic ironworks site. The Italian name is a slight modification from the Friulan, with "in Valromana" added, referring to an adjacent valley—which, however, is located a fair way off. The alternate Slovene denotation ''Bela Peč'', like the German name ''Weißenfels'', , refers to a historic castle erected by the Counts of Celje, owners of the area between 1418 and 1456, in the early 15th century. Geography The hamlet is located in the western Julian Alps, about east of the Tarvisio town centre and close to the tripoint where the borders of Slovenia, Austria, and Italy meet. It is a stop on highway SS 54, which leads from Tarvis ...
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Let's Go Our Own Way
''Let's Go Our Own Way'' ( sl, Gremo mi po svoje) is a 2010 Slovenian adventures youth film directed by Miha Hočevar, starring Jurij Zrnec, Tadej Koren Šmid, and Jure Kreft in the title roles. This film reached the biggest audience in premiere weekend in Slovenian cinema history. The film gathered record 18,686 visitors. Plot Film is talking about scouts who spend their free time in nature. Aleks is camping near Soča river together with his friends. Starešina, the scouting leader is taking everything too serious and that cause a lot of problems. And boys are a lot more interested in girls than camp. The movie was filmed in ideal Triglav National Park in Slovenia.http://www.film-sklad.si/index.php?module=strani&stranid=98&op=film&filmID=3334/ Filmski sklad short plot. November 11, 2010 Cast * Jurij Zrnec Jurij is a given name. Notable people with the name include: *Jurij Alschitz (born 1947), theatre director, theatre and acting theorist who has lived in Berlin since 1992 ...
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Manganese Nodule
Polymetallic nodules, also called manganese nodules, are mineral concretions on the sea bottom formed of concentric layers of iron and manganese hydroxides around a core. As nodules can be found in vast quantities, and contain valuable metals, deposits have been identified as a potential economic interest. Nodules vary in size from tiny particles visible only under a microscope to large pellets more than across. However, most nodules are between in diameter, about the size of hen's eggs or potatoes. Their surface textures vary from smooth to rough. They frequently have botryoidal (mammillated or knobby) texture and vary from spherical in shape to typically oblate (flying saucer), sometimes prolate (Rugby ball), or are otherwise irregular. The bottom surface, buried in sediment, is generally rougher than the top due to a different type of growth. Occurrence Nodules lie on the seabed sediment, often partly or completely buried. They vary greatly in abundance, in some cases ...
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Early Jurassic
The Early Jurassic Epoch (geology), Epoch (in chronostratigraphy corresponding to the Lower Jurassic series (stratigraphy), Series) is the earliest of three epochs of the Jurassic Period. The Early Jurassic starts immediately after the Triassic-Jurassic extinction event, 201.3 Ma (million years ago), and ends at the start of the Middle Jurassic 174.1 Ma. Certain rocks of marine origin of this age in Europe are called "Lias Group, Lias" and that name was used for the period, as well, in 19th-century geology. In southern Germany rocks of this age are called Black Jurassic. Origin of the name Lias There are two possible origins for the name Lias: the first reason is it was taken by a geologist from an England, English quarryman's dialect pronunciation of the word "layers"; secondly, sloops from north Cornwall, Cornish ports such as Bude would sail across the Bristol Channel to the Vale of Glamorgan to load up with rock from coastal limestone quarries (lias limestone from S ...
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Mountain Passes Of The Alps
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 ...
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Mountain Passes Of Slovenia
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 ...
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