|
Hardangervidda
Hardangervidda () is a mountain plateau ( Norwegian: ''vidde'') in central southern Norway, covering parts of Vestland, Telemark, and Buskerud counties. It is the largest plateau of its kind in Europe, with a cold year-round alpine climate, and one of Norway's largest glaciers, Hardangerjøkulen, is situated here. Much of the plateau is protected as part of Hardangervidda National Park. Hardangervidda is a popular tourist and leisure destination, and it is ideal for many outdoor activities. Geography and geology The plateau is the largest peneplain (eroded plain) in Europe, covering an area of about at an average elevation of . The highest point on the plateau is the Sandfloegga, which reaches a height of . The landscape of the Hardangervidda is characterised by barren, treeless moorland interrupted by numerous pools, lakes, rivers and streams. There are significant differences between the west side, which is dominated by rocky terrain and expanses of bare rock, and the e ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hardangervidda National Park
Hardangervidda National Park (, ), at , is Norway's largest national park. It spans from Numedal and Uvdal in the east and Røvelseggi and Ullensvang in the west across the Hardanger mountain plateau (Hardangervidda). Designated as a national park in 1981, today it serves as a popular tourist destination for activities such as hiking, climbing, fishing, and cross-country skiing. The Norwegian Mountain Touring Association (DNT) maintains a comprehensive network of huts and paths across Hardangervidda. The Bergen Line and the main Highway 7 cross the plateau. The park lies in Buskerud, Vestland, and Telemark counties. It has the southernmost stock of several arctic animals and plants. Its wild reindeer herds are among the largest in the world. Several hundred nomadic Stone Age settlements have been found in the area, most likely related to the migration of the reindeer. Ancient trails cross the plateau, linking western and eastern Norway; one example is the ''Nordmannsslepa'' lin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sub-Cambrian Peneplain
The sub-Cambrian peneplain is an ancient, extremely flat, erosion surface (peneplain) that has been exhumed and exposed by erosion from under Cambrian strata over large swathes of Fennoscandia. Eastward, where this peneplain dips below Cambrian and other Lower Paleozoic cover rocks. The outcrop, exposed parts of this peneplain are extraordinarily flat with relief of less than 20 m. The overlying cover rocks demonstrate that the peneplain was flooded by epicontinental sea, shallow seas during the Early Paleozoic. Being the oldest identifiable peneplain in its area the Sub-Cambrian peneplain qualifies as a primary peneplain. The surface was first identified by Arvid Högbom in a 1910 publication, with Sten Rudberg publishing the first extensive map in 1954. This mapping has been improved upon by Karna Lidmar-Bergström since the 1980s. Extent The Sub-Cambrian peneplain extends as an almost continuous belt along the eastern coast of Sweden for some 700 km from north to south. Near St ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hårteigen
Hårteigen is a characteristic mountain in Vestland county, Norway. It sits on and is visible from most parts of the vast Hardangervidda plateau. The mountain is located in the municipality of Ullensvang, and it is inside the Hardangervidda National Park. At an elevation of above sea level, the peak of Hårteigen rises above the surrounding plateau which is fairly level. It is located about northeast of the town of Odda. Name The first element is from the Old Norse word ''hárr'' which means 'grey' and the last element is related to the German verb ''zeigen'' which means 'show'. On the large and flat plateau of Hardangervidda this mountain was important for travellers to find the direction. See also *List of mountains of Norway There are 291 peaks in Norway with elevations of over above sea level and that have a topographic prominence of more than . The following list includes those 186 that have a topographic prominence of or more. The topographic isolation refers to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandfloegga
Sandfloegga or Sandfloeggi is a mountain in Ullensvang Municipality in southeastern Vestland county, Norway. It lies on the southern part of the vast Hardangervidda mountain plateau, and is the highest mountain on Hardangervidda when the bordering summits of Hardangerjøkulen and Folarskardnuten are omitted. The tall mountain lies inside Hardangervidda National Park, about north of the European route E134 highway. From the summit, the Folgefonna glacier is seen in the northwest, the mountain Hårteigen in the north, the Hallingskarvet mountain ridge and the glacier Hardangerjøkulen in the northeast, and the mountain Gaustatoppen in the east. See also *List of mountains of Norway There are 291 peaks in Norway with elevations of over above sea level and that have a topographic prominence of more than . The following list includes those 186 that have a topographic prominence of or more. The topographic isolation refers to ... References Ullensvang Mountains of Vestla ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Peneplain
In geomorphology and geology, a peneplain is a low-relief plain formed by protracted erosion. This is the definition in the broadest of terms, albeit with frequency the usage of peneplain is meant to imply the representation of a near-final (or penultimate) stage of fluvial erosion during times of extended tectonic stability. Peneplains are sometimes associated with the cycle of erosion theory of William Morris Davis, but Davis and other researchers have also used the term in a purely descriptive manner without any theory or particular genesis attached. Discussion 390px, Sketch of a hypothetical peneplain formation after an orogeny. The existence of some peneplains, and peneplanation as a process in nature, is not without controversy, due to a lack of contemporary examples and uncertainty in identifying relic examples. By some definitions, peneplains grade down to a base level represented by sea level, yet in other definitions such a condition is ignored. Geomorphologist K ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pliocene
The Pliocene ( ; also Pleiocene) is the epoch (geology), epoch in the geologic time scale that extends from 5.33 to 2.58See the 2014 version of the ICS geologic time scale million years ago (Ma). It is the second and most recent epoch of the Neogene Period in the Cenozoic, Cenozoic Era. The Pliocene follows the Miocene Epoch and is followed by the Pleistocene Epoch. Prior to the 2009 revision of the geologic time scale, which placed the four most recent major glaciations entirely within the Pleistocene, the Pliocene also included the Gelasian Stage, which lasted from 2.59 to 1.81 Ma, and is now included in the Pleistocene. As with other older geologic periods, the Stratum, geological strata that define the start and end are well-identified but the exact dates of the start a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Reindeer
The reindeer or caribou (''Rangifer tarandus'') is a species of deer with circumpolar distribution, native to Arctic, subarctic, tundra, taiga, boreal, and mountainous regions of Northern Europe, Siberia, and North America. It is the only representative of the genus ''Rangifer''. More recent studies suggest the splitting of reindeer and caribou into six distinct species over their range. Reindeer occur in both Animal migration, migratory and wiktionary:sedentary#Adjective, sedentary populations, and their herd sizes vary greatly in different regions. The tundra subspecies are adapted for extreme cold, and some are adapted for long-distance migration. Reindeer vary greatly in size and color from the smallest, the Svalbard reindeer (''R.'' (''t.'') ''platyrhynchus''), to the largest, Osborn's caribou (''R. t. osborni''). Although reindeer are quite numerous, some species and subspecies are in decline and considered Vulnerable species, vulnerable. They are unique among deer (Ce ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Telemark
Telemark () is a Counties of Norway, county and a current electoral district in Norway. Telemark borders the counties of Vestfold, Buskerud, Vestland, Rogaland and Agder. In 2020, Telemark merged with the county of Vestfold to form the county of Vestfold og Telemark. On 1 January 2024, the county of Telemark was re-established after Vestfold og Telemark was divided again. The name ''Telemark'' means the "March (territorial entity), mark of the Thelir", the ancient North Germanic peoples, North Germanic tribe that inhabited what is now known as Upper Telemark in the Migration Period and the Viking Age. In the Middle Ages, the agricultural society of Upper Telemark was considered the most violent region of Norway. Today, half of the buildings from medieval times in Norway are located here. The dialects spoken in Upper Telemark also retain more elements of Old Norse than those spoken elsewhere in the country. Upper Telemark is also known as the birthplace of skiing. The southern ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Buskerud
Buskerud () is a Counties of Norway, county and a current electoral district in Norway, bordering Akershus, Oslo, Innlandet, Vestland, Telemark and Vestfold. The region extends from the Oslofjord and Drammensfjorden in the southeast to Hardangervidda mountain range in the northwest. The county administration was in modern times located in Drammen. Buskerud was merged with Akershus and Østfold into the newly created Viken (county), Viken County on 1 January 2020. On 23 February 2022, the Viken County Council voted in a 49 against 38 decision to submit an application to the Norwegian government for a county demerger. Due to this, Buskerud (except the area forming the defunct municipalities of Røyken and Hurum) was re-established in 2024. Etymology The county was named after the old manor Buskerud Manor, Buskerud () (Biskopsrøysa) located on the west side of the Drammenselva, Drammen River in Åmot, Buskerud, Åmot, Modum municipality. The first element is the genitive case of ', ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vestland
Vestland is a Counties of Norway, county in Norway. The county is located in Western Norway, and its administrative centre is Bergen, where the executive and political leadership is based. The County governor (Norway), County Governor is based in Hermansverk. Vestland is one of two counties in Norway that have Nynorsk as their official written language form. Vestland was created on 1 January 2020, when the former counties of Hordaland and Sogn og Fjordane were merged. History Vestland county is a newly created county, but it has been inhabited for millennia. The area was made up of many petty kingdoms under the Gulating during the Middle Ages. The northern part was then known as ''Firdafylke'' (now the Fjordane region; Nordfjord-Sunnfjord), the central area was known as ''Sygnafylke'' (now the Sogn region), and the southern part was known as ''Hordafylke''. In the early 16th century, Norway was divided into four ''len''. The Bergenhus len was headquartered in Bergen and encompa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
