Mountain Ranges Of Norway
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Mountain Ranges Of Norway
The geography of Norway is dominated by vast mountain ranges broken up by valleys and fjords. Less than 10% of the country's area is arable land, arable, and the rest is mountainous. Glaciers are the major cause for erosion, so the terrain in the Norwegian mountains consists of plateaus and lakes with peaks. These areas have an abundant and diverse fauna and flora. The altitude of the treeline comes slowly down going to higher latitudes; in northern Finnmark, the treeline reaches sea level. The treeline is also lower near the coast, and higher on the eastern slopes of the mountains. Mountain ranges also form the main boundaries among Districts of Norway, Norway's districts. They typically run north-south. Several of the ranges have had road and railroad passes since historical times; some are newer; and many close over the winter. Norwegian mountain ranges provide some of the most attractive recreational areas, both during summer and winter. Cabins and trails are operated b ...
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Norway
Norway, officially the Kingdom of Norway, is a Nordic countries, Nordic country located on the Scandinavian Peninsula in Northern Europe. The remote Arctic island of Jan Mayen and the archipelago of Svalbard also form part of the Kingdom of Norway. Bouvet Island, located in the Subantarctic, is a Dependencies of Norway, dependency, and not a part of the Kingdom; Norway also Territorial claims in Antarctica, claims the Antarctic territories of Peter I Island and Queen Maud Land. Norway has a population of 5.6 million. Its capital and largest city is Oslo. The country has a total area of . The country shares a long eastern border with Sweden, and is bordered by Finland and Russia to the northeast. Norway has an extensive coastline facing the Skagerrak strait, the North Atlantic Ocean, and the Barents Sea. The unified kingdom of Norway was established in 872 as a merger of Petty kingdoms of Norway, petty kingdoms and has existed continuously for years. From 1537 to 1814, Norway ...
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Arable Land
Arable land (from the , "able to be ploughed") is any land capable of being ploughed and used to grow crops.''Oxford English Dictionary'', "arable, ''adj''. and ''n.''" Oxford University Press (Oxford), 2013. Alternatively, for the purposes of agricultural statistics, the term often has a more precise definition: A more concise definition appearing in the Eurostat glossary similarly refers to actual rather than potential uses: "land worked (ploughed or tilled) regularly, generally under a system of crop rotation". In Britain, arable land has traditionally been contrasted with pasturable land such as heaths, which could be used for sheep-rearing but not as farmland. Arable land is vulnerable to land degradation and some types of un-arable land can be enriched to create useful land. Climate change and biodiversity loss are driving pressure on arable land. By country According to the Food and Agriculture Organization of the United Nations, in 2013, the world's arable land amo ...
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Districts Of Norway
The country of Norway is historically divided into a number of districts. Many districts have deep historical roots, and only partially coincide with today's administrative units of counties of Norway, counties and municipalities of Norway, municipalities. The districts are defined by geographical features, often valleys, mountain ranges, fjords, plains, or coastlines, or combinations of the above. Many such regions were petty kingdoms up to the early Viking Age. Regional identity A high percentage of Norwegians identify themselves more by the district they live in or come from, than the formal administrative unit(s) whose jurisdiction they fall under. A significant reason for this is that the districts, through their strong geographical limits, have historically delineated the region(s) within which one could travel without too much trouble or expenditure of time and money (on foot or skis, by horse/ox-drawn cart or sleigh or dog sled, or by one's own small Watercraft rowing, ro ...
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Norwegian Mountain Touring Association
The Norwegian Trekking Association (, DNT) is a Norwegian association which maintains mountain trails and cabins in Norway. The association was founded on 21 January 1868 with the scope "to help and develop tourism in this country". Today the goal is to work for simple, secure and environmentally friendly outdoor activities. DNT has currently more than 300,000 individual members, and 57 local chapters. It also has several "honorary members", prominent people who have shown a keen interest in Norwegian nature and given the country publicity as a tourist destination, among them Kofi Annan and Katie Melua. The secretary-general of the association is Dag Terje Klarp Solvang. The mountains of Norway have always been utilised by the Norwegian people since the first Norwegians followed the reindeer when the ice cap retracted ten thousand years ago. DNT's first hut was Krokan by the Rjukan Rjukan () is a List of towns and cities in Norway, town in Tinn Municipality in Telemark count ...
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Trollheimen Mnt Trollhetta
Trollheimen is a mountain range in Møre og Romsdal and Trøndelag counties in central Norway. The mountain range is part of the Scandinavian Mountains. Etymology The name ('the home of the trolls') was proposed by Håkon Løken. It is used by Trondhjems Turistforening in the 1880s, and is considered a "tourist name" (there was no single name for the entire area before). Trollheimen is now the common name in Norway for this mountain range. Topography and climate Trollheimen is often considered the most varied of all mountain ranges in Norway. The mountains in the western part are alpine in form, with pointed peaks and typical river valleys. The mountains in the east are less steep with predominating rounded shapes, the valleys are wider and bear the mark of being created by glaciers. The climate differs from the more oceanic climate in the west to a considerably drier, continental climate in the eastern valleys, due to their being sheltered by mountains. The valleys in Troll ...
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Scandinavian Mountains
The Scandinavian Mountains or the Scandes is a mountain range that runs through the Scandinavian Peninsula. The western sides of the mountains drop precipitously into the North Sea and Norwegian Sea, forming the fjords of Norway, whereas to the northeast they gradually curve towards Finland. To the north they form the border between Norway and Sweden, reaching high at the Arctic Circle. The mountain range just touches northwesternmost Finland but are scarcely more than hills at their northernmost extension at the North Cape (). The mountains are relatively high for a range so young and are very steep in places; Galdhøpiggen in South Norway is the highest peak in mainland Northern Europe, at ; Kebnekaise is the highest peak on the Swedish side, at , whereas the slope of Halti is the highest point in Finland, at , although the peak of Halti is situated in Norway. The Scandinavian montane birch forest and grasslands terrestrial ecoregion is closely associated with the mou ...
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Caledonian Orogeny
The Caledonian orogeny was a mountain-building cycle recorded in the northern parts of the British Isles, the Scandinavian Caledonides, Svalbard, eastern Greenland and parts of north-central Europe. The Caledonian orogeny encompasses events that occurred from the Ordovician to Early Devonian, roughly 490–390 million years ago ( Ma). It was caused by the closure of the Iapetus Ocean when the Laurentia and Baltica continents and the Avalonia microcontinent collided. The orogeny is named for Caledonia, the Latin name for Scotland. The term was first used in 1885 by Austrian geologist Eduard Suess for an episode of mountain building in northern Europe that predated the Devonian period. Geologists like Émile Haug and Hans Stille saw the Caledonian event as one of several episodic phases of mountain building that had occurred during Earth's history.McKerrow ''et al.'' (2002) Current understanding has it that the Caledonian orogeny encompasses a number of tectonic phases th ...
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Geology Of Norway
The geology of Norway encompasses the history of Earth that can be interpreted by rock types found in Norway, and the associated sedimentological history of soils and rock types. The Norwegian mountains were formed around 400 million years ago (Ma) during the Caledonian orogeny. Precambrian Rocks of Archean age in Norway are confined to a few 10 km-scale areas within younger Metamorphic rock, metamorphic belts exposed on islands off the west coast of northern Norway and as smaller fragments locally in the Western Gneiss region in south-central Norway. Despite intense reworking during the Caledonian orogeny in some areas, three major belts can be recognised in the Proterozoic rocks of Norway, the Neoproterozoic and Mesoproterozoic Gothian and Sveconorwegian orogeny, Sveconorwegian, the Palaeoproterozoic Svecokarelian and the intervening Transscandinavian Igneous Belt of late Palaeoproterozoic age. About 1400 million years ago in the Mesoproterozoic extensional tectonics, te ...
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Mountain Ranges Of Norway
The geography of Norway is dominated by vast mountain ranges broken up by valleys and fjords. Less than 10% of the country's area is arable land, arable, and the rest is mountainous. Glaciers are the major cause for erosion, so the terrain in the Norwegian mountains consists of plateaus and lakes with peaks. These areas have an abundant and diverse fauna and flora. The altitude of the treeline comes slowly down going to higher latitudes; in northern Finnmark, the treeline reaches sea level. The treeline is also lower near the coast, and higher on the eastern slopes of the mountains. Mountain ranges also form the main boundaries among Districts of Norway, Norway's districts. They typically run north-south. Several of the ranges have had road and railroad passes since historical times; some are newer; and many close over the winter. Norwegian mountain ranges provide some of the most attractive recreational areas, both during summer and winter. Cabins and trails are operated b ...
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Lists Of Mountain Ranges
A list is a set of discrete items of information collected and set forth in some format for utility, entertainment, or other purposes. A list may be memorialized in any number of ways, including existing only in the mind of the list-maker, but lists are frequently written down on paper, or maintained electronically. Lists are "most frequently a tool", and "one does not ''read'' but only ''uses'' a list: one looks up the relevant information in it, but usually does not need to deal with it as a whole".Lucie Doležalová,The Potential and Limitations of Studying Lists, in Lucie Doležalová, ed., ''The Charm of a List: From the Sumerians to Computerised Data Processing'' (2009). Purpose It has been observed that, with a few exceptions, "the scholarship on lists remains fragmented". David Wallechinsky, a co-author of ''The Book of Lists'', described the attraction of lists as being "because we live in an era of overstimulation, especially in terms of information, and lists help us ...
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