Røvassdalen
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Røvassdalen
Røvassdalen is a valley in Rana Municipality in Nordland county, Norway. The upper part of the valley is located within the Saltfjellet–Svartisen National Park. The river of Røvassåga flows through the valley, and later it joins with the rivers Blakkåga and Svartisåga and further down with the Langvassåga. The karst cave Karst () is a topography formed from the dissolution of soluble carbonate rocks such as limestone and dolomite. It is characterized by features like poljes above and drainage systems with sinkholes and caves underground. There is some eviden ...s Setergrotta and Grønnligrotta are located in the valley. References Valleys of Nordland Rana, Norway {{nordland-geo-stub ...
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Setergrotta
Setergrotta (or Setergrotten) is a karst cave in Røvassdalen in Rana Municipality in Nordland county, 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 .... It has a total depth of and explored length of . It is probably connected to the nearby Grønligrotta. The cave contains large galleries and sediments from the latest ice age and younger. It was created 200,000–300,000 years ago. References Caves of Norway Karst caves Landforms of Nordland Rana, Norway Tourist attractions in Nordland {{nordland-geo-stub ...
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Grønnligrotta
Grønnligrotta is a marble karst cave in Rana Municipality in Nordland county, Norway. It is located in the valley of Røvassdalen, and was first explored in 1914. It has a total depth of and explored length of . It is probably connected to the nearby Setergrotta Setergrotta (or Setergrotten) is a karst cave in Røvassdalen in Rana Municipality in Nordland county, Norway Norway, officially the Kingdom of Norway, is a Nordic countries, Nordic country located on the Scandinavian Peninsula in Northern .... The cave is equipped with artificial lights and open for tourists. References Caves of Norway Marble caves Landforms of Nordland Rana, Norway Tourist attractions in Nordland {{nordland-geo-stub ...
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Nordland
Nordland (; , , , ) is one of the three northernmost Counties of Norway, counties in Norway in the Northern Norway region, bordering Troms in the north, Trøndelag in the south, Norrbotten County in Sweden to the east, Västerbotten County to the south-east, and the Atlantic Ocean (Norwegian Sea) to the west. The county was formerly known as ''Nordlandene amt''. The county administration is in the Bodø (town), town of Bodø. The remote Arctic island of Jan Mayen has been administered from Nordland since 1995. In the southern part of the county is Vega Municipality, Vega, listed on the UNESCO World Heritage Site list. Districts The county is divided into traditional districts. These are Helgeland in the south (south of the Arctic Circle), Salten in the centre, and Ofoten in the north-east. In the north-west lie the archipelagoes of Lofoten and Vesterålen. Geography Nordland is located along the northwestern coast of the Scandinavian Peninsula in Northern Norway. Due to t ...
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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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Norwegian Mapping Authority
The Norwegian Mapping Authority (NMA) () is Norway's national mapping agency, dealing with land surveying, geodesy Geodesy or geodetics is the science of measuring and representing the Figure of the Earth, geometry, Gravity of Earth, gravity, and Earth's rotation, spatial orientation of the Earth in Relative change, temporally varying Three-dimensional spac ..., hydrographic surveying, cadastre and cartography. The current director is Johnny Welle. Its headquarters are in Hønefoss in Ringerike Municipality. It is a public agency under the Ministry of Local Government and Regional Development. NMA was founded in 1773. The Norwegian Mapping Authority participates in research and development and cooperates with Norwegian industry and other government agencies in areas such as export-oriented measures. Tasks The NMA carries out the following tasks: *Define frameworks, methodologies and specifications for the Norwegian Spatial Data Infrastructure *Administrator and drivin ...
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Rana Municipality
or is a municipality in Nordland county, Norway. It is part of the Helgeland traditional region. The administrative centre of the municipality is the town of Mo i Rana, which houses the National Library of Norway. Other population centers in Rana include Båsmoen, Dunderland, Eiteråga, Flostrand, Hauknes, Myklebustad, Nevernes, Røssvoll, Selfors, Sjonbotn, Skonseng, Storforsheia, Utskarpen, and Ytteren. The municipality is the 4th largest by area out of the 357 municipalities in Norway (the largest municipality outside Troms and Finnmark counties). Rana is the 47th most populous municipality in Norway with a population of 25,994. This makes it the second largest municipality in Nordland county—and the third largest in North Norway. The municipality's population density is and its population has increased by 0.2% over the previous 10-year period. Rana was a part of the Terra Securities scandal in 2007 relating to some investments that were made by the m ...
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Saltfjellet–Svartisen National Park
Saltfjellet–Svartisen National Park () is a national park in Nordland county in Norway. It is located within the municipalities of Beiarn, Meløy, Rana, Rødøy, Saltdal, and Bodø. The park forms the centrepiece of a larger protected area of about , which includes the adjacent Gåsvatnan and Saltfjellet landscape protection areas and four small nature reserves. Saltfjellet–Svartisen features diverse landscapes ranging from coastal regions to alpine plateaux, birch-covered valleys, and tundra, with Svartisen—Scandinavia's second-largest glacier at roughly occupying the southwestern corner. The park's calcareous bedrock supports a remarkably rich flora, while traditional Sámi reindeer husbandry continues within its boundaries. The European route E6 highway and the Nordland Line railway both follow the southern and eastern borders around the park. Geography and ecology Saltfjellet–Svartisen was designated a national park by royal decree in 1989 and covers 2102 km2; t ...
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Langvassåga
Langvassåga is a river that flows out of the lake Langvatnet in Rana Municipality in Nordland county, Norway. It flows in a southeastern direction and almost immediately, it is joined by the river Røvassåga. It then continues a short distance southwards before joining the main river Ranelva, just south of the village of Røssvoll. The Langvassåga catchment area covers about . The river passes by the Mo i Rana Airport, Røssvoll. Media gallery Bridge at Langvassåga.JPG, Bridge on E6 above Langvassåga just before it meets Ranelva Langvassåga 01.JPG, Langvassåga west of the bridge Langvassåga 03.JPG, Langvassåga meets Ranelva east of the bridge See also *List of rivers in Norway The following are the 19 longest rivers of Norway, ranked by length: # Glomma, # Tana, # Pasvikelva and Ivalo, (109 km in Norway) # Numedalslågen, # Gudbrandsdalslågen and Vorma, # Drammensvassdraget (Drammenselva, # Hallingda ... References Rana, Norway Rivers ...
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Karst Cave
Karst () is a topography formed from the dissolution of soluble carbonate rocks such as limestone and 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 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 1 ...
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Store Norske Leksikon
The ''Great Norwegian Encyclopedia'' (, abbreviated ''SNL'') is a Norwegian-language online encyclopedia. It has several subdivisions, including the Norsk biografisk leksikon. The online encyclopedia is among the most-read Norwegian published sites, with up to 3.5 million unique visitors per month. Paper editions (1978–2007) The ''SNL'' was created in 1978, when the two publishing houses Aschehoug and Gyldendal merged their encyclopedias and created the company Kunnskapsforlaget. Up until 1978 the two publishing houses of Aschehoug and Gyldendal, Norway's two largest, had published ' and ', respectively. The respective first editions were published in 1906–1913 (Aschehoug) and 1933–1934 (Gyldendal). The slump in sales of paper-based encyclopedias around the turn of the 21st century hit Kunnskapsforlaget hard, but a fourth edition of the paper encyclopedia was secured by a grant of ten million Norwegian kroner from the foundation Fritt Ord in 2003. The f ...
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Valleys Of Nordland
A valley is an elongated low area often running between hills or mountains and typically containing a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In areas of limestone bedrock, dry valleys may also result from drainage now taking place underground rather than at the surface. Rift valleys arise principally from earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms that may be global in use or else applied only locally. Forma ...
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