Ã…rdalsfjord
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Ã…rdalsfjord
The Sognefjord or Sognefjorden (, en, Sogn Fjord), nicknamed the King of the Fjords ( no, Fjordenes konge), is the largest and deepest fjord in Norway. Located in Vestland county in Western Norway, it stretches inland from the ocean to the small village of Skjolden in the municipality of Luster. The fjord gives its name to the surrounding district of Sogn. The name is related to Norwegian word ''súg-'' "to suck", presumably from the surge or suction of the tidal currents at the mouth of the fjord. Geography The fjord runs through many municipalities: Solund, Gulen, Hyllestad, Høyanger, Vik, Sogndal, Lærdal, Aurland, Årdal, and Luster. The fjord reaches a maximum depth of below sea level, and the greatest depths are found in the central parts of the fjord near Høyanger. Sognefjord is more than deep for about of its length, from Rutledal to Hermansverk. Near its mouth, the bottom rises abruptly to a sill about below sea level. The seabed in Sognefjord is covered by ...
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Ã…rdal
Årdal is a municipality in Vestland county, Norway. It is located at the end of the Årdalsfjorden in the traditional district of Sogn. The village of Årdalstangen is the administrative center of the municipality. The other main village is Øvre Årdal. The municipality of Årdal was created in 1863 when it was separated from the municipality of Lærdal. Årdal is a modern industrial community, with ties to the old society of farming and fishing. It is surrounded by dramatic nature with high mountains and waterfalls. The climate is rather mild and with less rain than normal in the west part of Norway. Årdal is a good starting point to explore the wild nature of Jotunheimen National Park, and with summer and winter activities within its boundaries. The Vettisfossen waterfall (highest in Norway) is located within the municipality. The municipality is the 119th largest by area out of the 356 municipalities in Norway. Årdal is the 178th most populous municipality in Norway wit ...
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List Of Norwegian Fjords
This list of Norwegian fjords shows many of the fjords in Norway. In total, there are about 1,190 fjords in Norway and the Svalbard islands. The sortable list includes the lengths and locations of those fjords. Fjords See also * List of glaciers in Norway * Geography of Norway {{Authority control Fjords Norway Fjords In physical geography, a fjord or fiord () is a long, narrow inlet with steep sides or cliffs, created by a glacier. Fjords exist on the coasts of Alaska, Antarctica, British Columbia, Chile, Denmark, Germany, Greenland, the Faroe Islands, Icela ...
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Fjord
In physical geography, a fjord or fiord () is a long, narrow inlet with steep sides or cliffs, created by a glacier. Fjords exist on the coasts of Alaska, Antarctica, British Columbia, Chile, Denmark, Germany, Greenland, the Faroe Islands, Iceland, Ireland, Kamchatka, the Kerguelen Islands, Labrador, Newfoundland, New Zealand, Norway, Novaya Zemlya, Nunavut, Quebec, the Patagonia region of Argentina and Chile, Russia, South Georgia Island, Tasmania, United Kingdom, and Washington state. Norway's coastline is estimated to be long with its nearly 1,200 fjords, but only long excluding the fjords. Formation A true fjord is formed when a glacier cuts a U-shaped valley by ice segregation and abrasion of the surrounding bedrock. According to the standard model, glaciers formed in pre-glacial valleys with a gently sloping valley floor. The work of the glacier then left an overdeepened U-shaped valley that ends abruptly at a valley or trough end. Such valleys are fjords wh ...
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Gneiss
Gneiss ( ) is a common and widely distributed type of metamorphic rock. It is formed by high-temperature and high-pressure metamorphic processes acting on formations composed of igneous or sedimentary rocks. Gneiss forms at higher temperatures and pressures than schist. Gneiss nearly always shows a banded texture characterized by alternating darker and lighter colored bands and without a distinct cleavage. Gneisses are common in the ancient crust of continental shields. Some of the oldest rocks on Earth are gneisses, such as the Acasta Gneiss. Description Orthogneiss from the Czech Republic In traditional English and North American usage, a gneiss is a coarse-grained metamorphic rock showing compositional banding (gneissic banding) but poorly developed schistosity and indistinct cleavage. In other words, it is a metamorphic rock composed of mineral grains easily seen with the unaided eye, which form obvious compositional layers, but which has only a weak tendency to fracture ...
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Hiserøyna
Hiserøyna or Hisarøyna is an island in Gulen Municipality in Vestland county, Norway. The island lies about west of the mainland, and about west of the village of Eivindvik, the municipal centre of Gulen. The island is located south of the Sognesjøen and north of the Gulafjorden. In 2001, there were 43 residents living on the island. History The coastline is rocky and has several fjords which cut into the island. The southeast part of the island is dominated by the tall mountain ''Veten'', while the rest of the island is relatively flat with some marshy lowland areas. Most of the island is unsuitable for habitation. The island's inhabitants live in just a few farm areas: Nyhammaren (on the east coast), Stemnebø and Vilsvika (on the south coast), Hjartås (central part of the island, along a fjord), and Straume (on the northern coast). Transport In September 2013, a cable ferry connection was opened connecting Hisarøyna to the mainland. The regular ferry route take ...
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Sula, Solund
Sula (; also called Indre Solundøy ) is an island in Solund Municipality in Vestland county, Norway. The island is the main island of the municipality. The island is located at the mouth of the Sognefjorden on the north side of the Sognesjøen, about east of Holmebåen, the westernmost point in Norway. The largest village on the island is Hardbakke. The other main village area is Hersvikbygda on the northern part of the island. The island has a ferry service from the village of Krakhella on the island to the mainland village of Rutledal in Gulen Municipality and also to the village of Losnegard on the neighboring island of Losna, immediately to the east of Sula. Just southwest of Hardbakke, there is a bridge from Sula to the neighboring island of Steinsundøyna to the west. A narrow wide channel separates the two islands. Media gallery File:Solund 01.jpg, View of Sula island (looking southwest) File:Hardbakke.JPG, View of Hardbakke, on Sula island See also *List of ...
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Hurrungane
Hurrungane (also written ''Hurrungene'', ''Hurrungadn'', ''Horungane'') is a mountain range in the municipalities Luster and Årdal in Vestland county, Norway. The area is southwest in the larger mountain range Jotunheimen and is also part of Jotunheimen National Park. The range has some of the most alpine peaks in Norway, and has 23 peaks over (counting peaks with larger prominence than ). Several of the peaks are only accessible through climbing or glacier crossings. The starting point for hiking is the village of Turtagrø along the national tourist road, Sognefjellsvegen (RV55). The highest peaks in the area are * Store Skagastølstinden (Storen): * Store Styggedalstinden: * Jervvasstind (Gjertvasstind): * Sentraltind: * Vetle Skagastølstind: * Midtre Skagastølstind: * Skagastølsnebbet: * Store Austanbotntind: Name ''Hurrungane'' is the finite plural of a word ''hurrung''. ''Hurrungen'', the finite singular of the same word, is the names of two mountains in Rau ...
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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#Glaciology, ablation over many years, often Century, centuries. It acquires distinguishing features, such as Crevasse, crevasses and Serac, seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on every continent other than the Australian mainland, including Oceania's high-latitude oceanic island countries such as New Zealand. Between lati ...
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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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Strandflat
Strandflat ( no , strandflate) is a landform typical of the Norwegian coast consisting of a flattish erosion surface on the coast and near-coast seabed. In Norway, strandflats provide room for settlements and agriculture, constituting important cultural landscapes. The shallow and protected waters of strandflats are valued fishing grounds that provide sustenance to traditional fishing settlements. Outside Norway proper, strandflats can be found in other high-latitude areas, such as Antarctica, Alaska, the Canadian Arctic, the Russian Far North, Greenland, Svalbard, Sweden and Scotland. The strandflats are usually bounded on the landward side by a sharp break in slope, leading to mountainous terrain or high plateaux. On the seaward side, strandflats end at submarine slopes. The bedrock surface of strandflats is uneven and tilts gently towards the sea. The concept of a strandflat was introduced in 1894 by Norwegian geologist Hans Reusch. Norwegian strandflat Characteristics Str ...
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Aurlandsfjorden
Aurlandsfjord ( no, Aurlandsfjorden, ) is a fjord in Vestland county, Norway. The fjord flows through the municipalities of Aurland, Vik, and Lærdal. The long fjord is a branch off of the main Sognefjorden, Norway's longest fjord. The fjord is deep and narrow, reaching a depth of about below sea level, and its width is generally less than wide. About south of the mouth of the fjord, the Nærøyfjord branches off from it to the west. The village of Flåm sits at the innermost part of the Aurlandsfjord; other villages along the fjord are Aurlandsvangen and Undredal. Most of the fjord is surrounded by up to tall, steep mountains with little habitation along the fjord except for in a few small valleys. Large parts of the fjord are included in the Nærøyfjord section of the ''West Norwegian Fjords'' UNESCO world heritage site. Gallery File:Aurlandsfjorden frå Snøvegen.jpg, Aurlandsfjorden as seen from Aurland mountain road File:Aurlandsfjorden from Stegastein.jpg, Seen ...
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Losna (island)
Losna is an island in the municipality of Solund in Vestland county, Norway. The island lies at the mouth of the Sognefjorden, on the north side of the Sognesjøen. The Tollesundet strait lies between the island and the mainland of Hyllestad to the east and the Krakhellasundet strait lies between the island and the nearby island of Sula to the west. The island of Sula sits only about to the west. The highest point on the very rocky island is the tall mountain Meinova on the northern end of the island. The island's residents live on the southeastern side of the island, in and around the small village of Losnegard. The only access to the island is by boat, and there are ferry routes from Rutledal to the south in Gulen and to the village of Krakhella on the island of Sula to the west. The island was part of the municipality of Gulen until 1964 when it was administratively transferred to the municipality of Solund. At the beginning of the 1900s, there were about 100 permane ...
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