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Jutulhogget (Oppland)
Jutulhogget is a small canyon in Sel Municipality in Innlandet county, Norway. The long canyon is located just southwest of the Rondvassbu hiking cabins at the south end of the lake Rondvatnet inside Rondane National Park Rondane National Park ( no, Rondane nasjonalpark) is the oldest national park in Norway, having been established on 21 December 1962. The park is located in Innlandet county, in the municipalities of Dovre, Folldal, Sel, Nord-Fron, Sør-Fron, Stor .... The highest parts of the canyon walls reach approximately high. The canyon was dug out by large amounts of water at the end of the last ice age. References Sel Canyons and gorges of Norway Geology of Norway Landforms of Innlandet {{Innlandet-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Innlandet
Innlandet is a county in Norway. It was created on 1 January 2020 with the merger of the old counties of Oppland and Hedmark (the municipalities of Jevnaker and Lunner were transferred to the neighboring county of Viken on the same date). The new county has an area of , making it the second largest county in Norway after Troms og Finnmark county. The county name translates to "The Inland" which reflects that the county is the only landlocked county in Norway. The county covers approximately 17% of the total area of the mainland area of Norway. It stretches from the Viken county and the Oslo region in the south to Trøndelag county in the north. In the northwest, the county borders Møre og Romsdal and the Vestland county in the west. To the east the county borders the Swedish counties of Värmland and Dalarna. The northern and western areas of the county are dominated by the mountainous areas Rondane, Dovrefjell and Jotunheimen. The Galdhøpiggen mountain is located within t ... [...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] |
Canyon
A canyon (from ; archaic British English spelling: ''cañon''), or gorge, is a deep cleft between escarpments or cliffs resulting from weathering and the erosion, erosive activity of a river over geologic time scales. Rivers have a natural tendency to cut through underlying surfaces, eventually wearing away rock layers as sediments are removed downstream. A river bed will gradually reach a baseline elevation, which is the same elevation as the body of water into which the river drains. The processes of weathering and erosion will form canyons when the river's River source, headwaters and estuary are at significantly different elevations, particularly through regions where softer rock layers are intermingled with harder layers more resistant to weathering. A canyon may also refer to a rift between two mountain peaks, such as those in ranges including the Rocky Mountains, the Alps, the Himalayas or the Andes. Usually, a river or stream carves out such splits between mountains. Examp ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canyon
A canyon (from ; archaic British English spelling: ''cañon''), or gorge, is a deep cleft between escarpments or cliffs resulting from weathering and the erosion, erosive activity of a river over geologic time scales. Rivers have a natural tendency to cut through underlying surfaces, eventually wearing away rock layers as sediments are removed downstream. A river bed will gradually reach a baseline elevation, which is the same elevation as the body of water into which the river drains. The processes of weathering and erosion will form canyons when the river's River source, headwaters and estuary are at significantly different elevations, particularly through regions where softer rock layers are intermingled with harder layers more resistant to weathering. A canyon may also refer to a rift between two mountain peaks, such as those in ranges including the Rocky Mountains, the Alps, the Himalayas or the Andes. Usually, a river or stream carves out such splits between mountains. Examp ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sel Municipality
Sel is a List of municipalities of Norway, municipality in Innlandet county, Norway. It is located in the Traditional districts of Norway, traditional district of Gudbrandsdal. The administrative centre of the municipality is the List of cities in Norway, town of Otta, Norway, Otta. The municipality also includes several notable villages including Bjølstad, Dale, Sel, Dale, Høvringen, Nord-Sel, Sandbumoen, Sjoa (village), Sjoa, and Skogbygda, Sel, Skogbygda. The municipality is the 130th largest by area out of the 356 municipalities in Norway. Sel is the 172nd most populous municipality in Norway with a population of 5,531. The municipality's population density is and its population has decreased by 7.7% over the previous 10-year period. General information The new municipality of Sel was established on 1 January 1908 when Vågå Municipality was divided into three. The northeastern part became the new Sel Municipality (population: 2,287), the southeastern part became the ne ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rondvatnet
Rondvatnet is a lake in Sel Municipality in Innlandet county, Norway. The lake is a long, narrow lake in Rondane National Park, about northeast of the town of Otta. The Norwegian Mountain Touring Association's tourist cabins at Rondvassbu are located at the southern end of this lake. Rondvatnet separates the eastern part of Rondane from the western part which is the site of Smiubelgen. During the summer season, there is boat service on the lake transporting hikers between the southern and northern end. The Jutulhogget canyon is located near the southern end of the lake. Name The lake is named Rondvatnet which directly translates to "the Rond water". The first part of the lake's name is ''rond'' which was probably the original name of the long and narrow lake. The Old Norse form of the name was just ''Rǫnd'', derived from the word ''rǫnd'' which means 'stripe' or 'edge' (referring to the long and narrow form of the lake). The last part of the name is ''vatnet'' which means ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rondane National Park
Rondane National Park ( no, Rondane nasjonalpark) is the oldest national park in Norway, having been established on 21 December 1962. The park is located in Innlandet county, in the municipalities of Dovre, Folldal, Sel, Nord-Fron, Sør-Fron, Stor-Elvdal, and Ringebu. The park contains ten peaks above , with the highest being Rondeslottet at an altitude of . The park is an important habitat for herds of wild reindeer. The park was enlarged in 2003, and now covers an area of . Rondane lies just to the east of the Gudbrandsdalen valley and two other mountain areas, Dovre and Jotunheimen are nearby. Dovre National Park lies a very short distance to the north of this park. Geography Rondane is a typical high mountain area, with large plateaus and a total of ten peaks above . The highest point is Rondeslottet ("The Rondane Castle") at an altitude of . The lowest point is just below the tree line, which is located at approximately above sea level. The climate is mild but relatively ari ... [...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] |
Kunnskapsforlaget
Kunnskapsforlaget () is a Norwegian publishing company based in Oslo. Kunnskapsforlaget was established in 1975, as a partnership between H. Aschehoug & Co. (W. Nygaard) and Gyldendal Norsk Forlag. The purpose was to co-operate on publishing encyclopaedias and dictionaries. The first volume of Store norske leksikon (SNL) was published in 1978. A total of four editions was published (the last one in 2004), before the online version was transferred to Institusjonen Fritt Ord og Sparebankstiftelsen DnB in 2011. Kunnskapsforlaget is the largest dictionary publisher in Norway. They publish both printed books, and digital dictionaries that are available through the online service Ordnett (launched in 2004). Their main languages are English and Norwegian, but they also have dictionaries in 21 other languages. In September 2018, Gyldendal Norsk Forlag became the single owner of the company. As of 2018, the publisher has eight full-time employees. The CEO is Thomas Nygaard Thomas m ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canyons And Gorges Of Norway
A canyon (from ; archaic British English spelling: ''cañon''), or gorge, is a deep cleft between escarpments or cliffs resulting from weathering and the erosive activity of a river over geologic time scales. Rivers have a natural tendency to cut through underlying surfaces, eventually wearing away rock layers as sediments are removed downstream. A river bed will gradually reach a baseline elevation, which is the same elevation as the body of water into which the river drains. The processes of weathering and erosion will form canyons when the river's headwaters and estuary are at significantly different elevations, particularly through regions where softer rock layers are intermingled with harder layers more resistant to weathering. A canyon may also refer to a rift between two mountain peaks, such as those in ranges including the Rocky Mountains, the Alps, the Himalayas or the Andes. Usually, a river or stream carves out such splits between mountains. Examples of mountain-type c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 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, the Palaeoproterozoic Svecokarelian and the intervening Transscandinavian Igneous Belt of late Palaeoproterozoic age. About 1400 million years ago in the Mesoproterozoic tectonic extension and continental magmatism led to the formatio ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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