Jutulhogget (Østerdalen)
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Jutulhogget (Østerdalen)
Jutulhogget is a long dry canyon in the municipalities of Alvdal and Rendalen in Innlandet county, 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 t .... The canyon was created by the rupture of the dam of a proglacial lake and the force of the rushing water leaving the lake carved out the canyon. The canyon was protected as a nature reserve in 1959. The steep walls of the canyon range from in height. The canyon was formed at the end of the last Ice Age, around  years ago. The proglasial lake Nedre Glomsjø was dammed up by glaciers stopping the water from running southward. As the amount of meltwater rose, it eventually broke through its earthen boundaries and formed a new outlet heading eastward through a weakness zone in the bedrock. The lake drained through to th ...
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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 ...
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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 ...
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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 ...
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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 ...
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Alvdal
Alvdal is a municipality in Innlandet county, Norway. It is located in the traditional district of Østerdalen. The administrative centre of the municipality is the village of Alvdal. Other villages include Barkald, Plassmoen, and Strømmen. The municipality is located to the south of Tynset, north and west of Rendalen, north of Stor-Elvdal, and east of Folldal. The Rørosbane railway and the Norwegian National Road 3 both pass through Alvdal. The municipality is the 124th largest by area out of the 356 municipalities in Norway. Alvdal is the 260th most populous municipality in Norway with a population of 2,445. The municipality's population density is and its population has increased by 0.6% over the previous 10-year period. General information In 1864, the parish of ''Lille-Elvdal'' (later renamed "Alvdal") was separated from Tynset Municipality to become a separate municipality of its own. Initially, the new municipality had a population of 3,216. On 1 January 1914 ...
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Rendalen
Rendalen is a municipality in Innlandet county, Norway. It is located in the traditional district of Østerdalen. The administrative centre of the municipality is the village of Bergset. Other villages in the municipality include Hanestad, Otnes, Sjølisand, Unset, Åkre, and Åkrestrømmen. The municipality is the 13th largest by area out of the 356 municipalities in Norway. Rendalen is the 294th most populous municipality in Norway with a population of 1,722. The municipality's population density is and its population has decreased by 12.1% over the previous 10-year period. General information The municipality of Rendalen was established on 1 January 1965 when the old municipalities of Ytre Rendal (population: 1,913) and Øvre Rendal (population: 1,629) were merged. On 1 January 1984, the unpopulated Spekedalen valley was transferred from Tynset Municipality to Rendalen. Name The municipality is named after the Rendalen valley ( non, Reindalr) which is located within ...
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Proglacial Lake
In geology, a proglacial lake is a lake formed either by the damming action of a moraine during the retreat of a melting glacier, a glacial ice dam, or by meltwater trapped against an ice sheet due to isostatic depression of the crust around the ice. At the end of the last ice age about 10,000 years ago, large proglacial lakes were a widespread feature in the northern hemisphere. Moraine-dammed The receding glaciers of the tropical Andes have formed a number of proglacial lakes, especially in the Cordillera Blanca of Peru, where 70% of all tropical glaciers are. Several such lakes have formed rapidly during the 20th century. These lakes may burst, creating a hazard for zones below. Many natural dams (usually moraines) containing the lake water have been reinforced with safety dams. Some 34 such dams have been built in the Cordillera Blanca to contain proglacial lakes. Several proglacial lakes have also formed in recent decades at the end of glaciers on the eastern side of Ne ...
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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 ...
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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 ...
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Weichselian Glaciation
The Weichselian glaciation was the last glacial period and its associated glaciation in northern parts of Europe. In the Alpine region it corresponds to the Würm glaciation. It was characterized by a large ice sheet (the Fenno-Scandian ice sheet) that spread out from the Scandinavian Mountains and extended as far as the east coast of Schleswig-Holstein, northern Poland and Northwest Russia. This glaciation is also known as the Weichselian ice age (german: Weichsel-Eiszeit), Vistulian glaciation, Weichsel or, less commonly, the Weichsel glaciation, Weichselian cold period (''Weichsel-Kaltzeit''), Weichselian glacial (''Weichsel-Glazial''), ''Weichselian Stage'' or, rarely, the Weichselian complex (''Weichsel-Komplex''). In Northern Europe it was the youngest of the glacials of the Pleistocene ice age. The preceding warm period in this region was the Eemian interglacial. The last cold period began about 115,000 years ago and ended 11,700 years ago. Its end corresponds with the end o ...
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Nedre Glomsjø
Nedre may refer to: *Nedre Eggedal, village in Sigdal municipality, Norway *Nedre Eiker, municipality in Buskerud county, Norway *Nedre Elvehavn, borough of Trondheim, Norway *Nedre Fagervollvatnet, Norwegian lake that lies in Rana municipality in Nordland *Nedre Fiplingvatnet, Norwegian lake that lies in Grane municipality in Nordland *Nedre Heimdalsvatnet, lake which lies in Vågå and Øystre Slidre municipalities in Oppland county, Norway *Nedre Roasten, lake in Femundsmarka National Park in Sør-Trøndelag county, Norway *Nedre Stjørdal, former municipality in Nord-Trøndelag county, Norway *Nedre Veikvatnet or is a lake that lies in the municipality of Sørfold in Nordland county, Norway Norway, officially the Kingdom of Norway, is a Nordic country in Northern Europe, the mainland territory of which comprises the western and northernmo ...
, Norwegian lake that lies in Sørfold municipality in Nordland {{Disambiguation ...
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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 ...
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