Høgste Breakulen
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Høgste Breakulen
Høgste Breakulen is the highest point on the Norwegian glacier Jostedalsbreen. It is inside the Jostedalsbreen National Park on the border of the municipalities of Stryn and Luster in Vestland county, Norway. Lodalskåpa, a nunatak to the northwest, and Brenibba, another nunatak that is to the northwest, are both higher than Høgste Breakulen, but they are not covered by the glacier. 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 10 meters. The following list includes those 186 that have a topographic prominence of 50 meters or more. The topographic i ... References External links http://www.westcoastpeaks.com/Peaks/hbreakulen.html Mountains of Vestland Stryn Luster, Norway {{Vestland-mountain-stub ...
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Vestland
Vestland is a county in Norway established on 1 January 2020. The county is located in Western Norway and it is centred around the city of Bergen, Norway's second largest city. The administrative centre of the county is the city of Bergen, where the executive and political leadership is based, but the County Governor is based in Hermansverk. The county is one of two counties in Norway that have Nynorsk as their official written language form (the others are neutral as to which form people use). Vestland was created in 2020 when the former counties of Hordaland and Sogn og Fjordane (with the exception of Hornindal municipality, which became part of Volda municipality in Møre og Romsdal county) were merged. History Vestland county is a newly created county, but it has been inhabited for centuries. The area was made up of many petty kingdoms under the Gulating during the Middle Ages. The northern part was the known as ''Firdafylke'' (now the Fjordane region; Nordfjord-Sunnfjord), ...
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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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Breheimen
Breheimen is a mountain range in the Innlandet and Vestland counties in Norway. The area lies west of the Jotunheimen mountain range. The mountain range lies to the northwest of the Sognefjellsvegen road, north of the Sognefjorden, south of the Nordfjorden and Norwegian National Road 15, and east of Norwegian National Road 5 and European route E39. The mountain range includes Jostedalsbreen National Park and Breheimen National Park. The name ''Breheimen'' means "home of the glaciers", since it has many glaciers, including Norway's largest glacier, Jostedalsbreen. Other glaciers in the range include Harbardsbreen and Spørteggbreen. Some of the major mountains in the area include Skåla, Lodalskåpa, Høgste Breakulen, Tverrådalskyrkja, Hestbrepiggene, and Brenibba. The region is home to several large lakes such as Austdalsvatnet and Styggevatnet Styggevatnet is a glacial lake from the glacier Jostedalsbreen in Luster Municipality in Vestland county, Norway. The lake lie ...
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Jostedalsbreen
Jostedal Glacier or is the largest glacier in continental Europe. It is in Vestland county in Western Norway. Jostedalsbreen lies in the municipalities of Luster, Norway, Luster, Sogndal, Sunnfjord (municipality), Sunnfjord, and Stryn. The highest peak in the area is Lodalskåpa at a height of . History In 1906, work was being done on footpaths that could accommodate tourists. Geography The Jostedal Glacier has a total area of . The highest point is Høgste Breakulen at above mean sea level. Branches of the glacier reach down into the valleys, for instance Bøyabreen in Fjærland and Nigardsbreen, both at above sea level. The thickest part of the glacier is . Jostedalsbreen has a length of a little more than and it is a part of the Jostedalsbreen National Park, which was established in 1991. The glacier covers over half of the national park. The glacier is maintained by the high snowfall rates in the region, not the cold temperatures. This means the glacier has high melt ...
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Jostedalsbreen National Park
Jostedalsbreen National Park ( no, Jostedalsbreen nasjonalpark) is a national park in Norway that encompasses the largest glacier on the European mainland, Jostedalsbreen. The park was established by royal decree on 25 October 1991, and then in 1998, it was enlarged to the northwest. The park now covers , with the glaciers covering about of the park. Location The park lies in the municipalities of Luster, Sogndal, Gloppen, Sunnfjord, and Stryn, all of which are in Vestland county. There are three museums and also visitors centers: the Breheimsenteret in Jostedalen, Jostedalsbreen nasjonalparksenter in Oppstryn (Stryn Municipality) and Norsk bremuseum in Fjærland (Sogndal Municipality). Topography The highest peak in the park is Lodalskåpa at . The glacier's highest point, Brenibba, lies above sea level while its lowest point is above sea level. The glacier has shrunk in recent years, and there are ruins of farms that were overtaken by the glacier in 1750. Name The par ...
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Stryn
Stryn is a municipality in the county of Vestland, Norway. It is located in the traditional district of Nordfjord. The administrative center of the municipality is the village of Stryn. The municipality is located along the innermost part of the Nordfjorden. Some of the main villages in Stryn include Loen, Innvik, Utvik, Randabygda, Olden, and Flo. Farming, forestry, fruit growing, animal breeding for furs, small manufacturing industries, tourism, and the service trades provide the main occupations. The wide river Stryneelva enters the village of Stryn from the east after meandering through the fertile Stryn Valley, from the large lake Oppstrynsvatn. The Jostedalsbreen National Park Centre is situated on the shore of this lake. At the east end of the lake, the road enters the narrower Hjelledalen and shortly zigzags up some to Ospeli and the entrance of the first of the three tunnels of the mountain highway ( Riksvei 15) leading to Geiranger and Grotli. Stryn is kno ...
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Luster, Norway
Luster is a municipality in Vestland county, Norway. It is located at the end of the Sognefjorden in the traditional district of Sogn. The administrative centre is the village of Gaupne. Other villages in Luster include Fortun, Hafslo, Indre Hafslo, Jostedal, Luster, Nes, Ornes, Skjolden, Solvorn, and Veitastrond. Luster is centered around the inner branch of the Sognefjord, which is called the Lustrafjorden. Its landscape includes fjords, steep mountains, water-abundant waterfalls, blue glaciers, and valleys. Both Jostedalsbreen National Park and Breheimen National Park are partially located in this municipality. The Sognefjellsvegen road goes over a mountain pass in eastern Luster. The municipality is the 17th largest by area out of the 356 municipalities in Norway. Luster is the 177th most populous municipality in Norway with a population of 5,246. The municipality's population density is and its population has increased by 4.4% during the previous 10-year period. I ...
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Lodalskåpa
Lodalskåpa is the highest nunatak on the Norwegian glacier Jostedalsbreen. It is located on the border between the municipalities of Stryn and Luster in Vestland county, Norway, within Jostedalsbreen National Park. The tall Lodalskåpa is located north of Brenibba and northeast of Høgste Breakulen mountain. The lakes Austdalsvatnet and Styggevatnet lie about to the east. The first ascent may have happened in 1820 by Gottfried Bohr. The easiest route to climb Lodalskåpa starts in the village of Bødalen in Stryn, then going up Brattebakken mountain to the Bohr glacier ( no, Bohrsbreen). Around the southern summit to the col, then scrambling to the main summit, approximately one rope length. Name The first element is the genitive case of the name of the valley Lodalen, the last element is the finite form of ''kåpe'' which means "coat" (here used metaphorically about the glacier surrounding the top–see also Snøhetta). The name of the valley is a compound of ''lo ...
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Nunatak
A nunatak (from Inuit ''nunataq'') is the summit or ridge of a mountain that protrudes from an ice field or glacier that otherwise covers most of the mountain or ridge. They are also called glacial islands. Examples are natural pyramidal peaks. When rounded by glacial action, smaller rock promontories may be referred to as rognons. The word is of Greenlandic origin and has been used in English since the 1870s. Description The term is typically used in areas where a permanent ice sheet is present and the nunataks protrude above the sheet.J. J. Zeeberg, ''Climate and Glacial History of the Novaya Zemlya Archipelago, Russian Arctic''. pp. 82–84 Nunataks present readily identifiable landmark reference points in glaciers or ice caps and are often named. While some nunataks are isolated, sometimes they form dense clusters, such as Queen Louise Land in Greenland. Nunataks are generally angular and jagged, which hampers the formation of glacial ice on their tops, although snow can a ...
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Brenibba
Brenibba is a nunatak protruding from the north end of the Jostedalsbreen glacier in the Breheimen mountain range. It is located in the municipality of Luster in Vestland county, Norway. Brenibba is south of Lodalskåpa and northeast of Høgste Breakulen. It is part of the Jostedalsbreen National Park. The lakes Austdalsvatnet and Styggevatnet are located west of Brenibba. Name The first element is ''bre'' which means "glacier A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its ablation over many years, often centuries. It acquires distinguishing features, such as ..." and the last element is the finite form of ''nibbe'' which means "mountain peak". References

Mountains of Vestland Luster, Norway {{Vestland-mountain-stub ...
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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 10 meters. The following list includes those 186 that have a topographic prominence of 50 meters or more. The topographic isolation refers to the shortest ''horizontal'' distance one would have to travel to find a higher summit. Location of peaks Most of these peaks are in the municipalities of Lom, Skjåk, Luster, and Vågå, connected to the mountain chain that reaches its prominence with Jotunheimen. There are also several peaks in Dovrefjell, Rondane, Dovre, Lesja, and Folldal that also reach above 2000 meters. All the peaks are to be found in 14 topographical maps ( Norge 1:50000) published by the Norwegian government cartography office, of which 21 peaks are in ''1518 II Galdhøpiggen'', 18 in ''1618 III Glittertinden'', and 13 in ''1617 IV Gjende''. The northernmost is in the Dovre area, meaning there are no 2000 m peaks in northern Norway, even thoug ...
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Mountains Of Vestland
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ...
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