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Røvassdalen
Røvassdalen is a valley in the municipality of Rana 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 caves Setergrotta and Grønligrotta Grønligrotta (or Grønligrotten) is a karst cave in the municipality of Rana in Nordland Nordland (; smj, Nordlánnda, sma, Nordlaante, sme, Nordlánda, en, Northland) is a county in Norway in the Northern Norway region, the least populou ... are located in the valley. References Valleys of Nordland Rana, Norway {{nordland-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Grønligrotta
Grønligrotta (or Grønligrotten) is a karst cave in the municipality of Rana in Nordland Nordland (; smj, Nordlánnda, sma, Nordlaante, sme, Nordlánda, en, Northland) is a county in Norway in the Northern Norway region, the least populous of all 11 counties, bordering Troms og Finnmark in the north, Trøndelag in the south, N ..., 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. The cave is equipped with artificial lights and open for tourists. References Caves of Norway Karst caves Landforms of Nordland Rana, Norway Tourist attractions in Nordland {{nordland-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Setergrotta
Setergrotta (or Setergrotten) is a karst cave in Røvassdalen in the municipality of Rana in Nordland, Norway. It has a total depth of 50 meters and explored length of 2.4 kilometers. It is probably connected to the nearby Grønligrotta Grønligrotta (or Grønligrotten) is a karst cave in the municipality of Rana in Nordland Nordland (; smj, Nordlánnda, sma, Nordlaante, sme, Nordlánda, en, Northland) is a county in Norway in the Northern Norway region, the least populou .... The cave contains large galleries and sediments from the latest ice age and younger. It was created 2–300,000 years ago. References Caves of Norway Karst caves Landforms of Nordland Rana, Norway Tourist attractions in Nordland {{nordland-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nordland
Nordland (; smj, Nordlánnda, sma, Nordlaante, sme, Nordlánda, en, Northland) is a county in Norway in the Northern Norway region, the least populous of all 11 counties, bordering Troms og Finnmark 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 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, 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 pe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Norway
Norway, officially the Kingdom of Norway, is a Nordic country in Northern Europe, the mainland territory of which comprises the western and northernmost portion of the Scandinavian Peninsula. The remote Arctic island of Jan Mayen and the archipelago of Svalbard also form part of Norway. Bouvet Island, located in the Subantarctic, is a dependency of Norway; it also lays claims to the Antarctic territories of Peter I Island and Queen Maud Land. The capital and largest city in Norway is Oslo. Norway has a total area of and had a population of 5,425,270 in January 2022. The country shares a long eastern border with Sweden at a length of . It is bordered by Finland and Russia to the northeast and the Skagerrak strait to the south, on the other side of which are Denmark and the United Kingdom. Norway has an extensive coastline, facing the North Atlantic Ocean and the Barents Sea. The maritime influence dominates Norway's climate, with mild lowland temperatures on the se ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rana, Norway
Rana 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, Mæla, Myklebustad, Nevernes, Røssvoll, Selfors, Skonseng, Storforshei, Utskarpen, and Ytteren. The municipality is the 4th largest by area out of the 356 municipalities in Norway (the largest municipality outside Troms og Finnmark county). Rana is the 45th most populous municipality in Norway with a population of 26,092. 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 1.7% 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 municipality. Gen ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saltfjellet–Svartisen National Park
Saltfjellet–Svartisen National Park ( no, Saltfjellet–Svartisen nasjonalpark) is a national park in Nordland county in Norway. It is located within the municipalities of Beiarn, Meløy, Rana, Rødøy, Saltdal, and Bodø. European route E6 and the Nordland Line both follow the southern and eastern borders around the park. The park's eastern border is the Norway-Sweden border and a portion of this border is shared with the Vindelfjällen Nature Reserve which lies in Sweden. At , it is one of the largest national parks in Norway. It is also one of the most varied, since it includes both alpine mountain formations with glacier tongues, as well as gently sloping mountain plateaus and forested valleys. The national park encompasses parts of the Saltfjellet mountain range. The Svartisen glacier is a central part of the park. There are also many Sami Acronyms * SAMI, ''Synchronized Accessible Media Interchange'', a closed-captioning format developed by Microsoft * Saudi Ara ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Langvassåga
Langvassåga is a river that flows out of the lake Langvatnet in the municipality of Rana 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, # Pasvikelva and Ivalo, (109 km in Norway) # Numedalslågen, # Gudbrandsdalslågen and Vorma, # Tana, # Drammensvassdraget (Drammenselva, # Skiensvassdrag ... References Rana, Norway ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Karst Cave
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] |
Store Norske Leksikon
The ''Great Norwegian Encyclopedia'' ( no, Store Norske Leksikon, abbreviated ''SNL''), is a Norwegian-language online encyclopedia. The online encyclopedia is among the most-read Norwegian published sites, with more than two 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 1907–1913 (Aschehoug) and 1933–1934 (Gyldendal). The slump in sales for 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 fourth edition consisted of 16 volumes, a t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Valleys Of Nordland
A valley is an elongated low area often running between Hill, hills or Mountain, mountains, which will typically contain 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 glacier, glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glaciation, 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 karst, areas of limestone bedrock, dry valleys may also result from drainage now taking place cave, underground rather than at the surface. Rift valleys arise principally from tectonics, earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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