Dalsfjorden (Sunnmøre)
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Dalsfjorden (Sunnmøre)
Dalsfjorden is a fjord in Volda Municipality in Møre og Romsdal county, Norway. The long fjord flows north into the Voldsfjorden. There are several small villages along the shores of the fjord, the largest of which are Dravlaus on the western shore, Steinsvika at the southern end of the fjord, and Dalsbygda on the eastern shore. County Road 40 runs around the shoreline of the whole fjord. The fjord averages about wide and it reaches a depth of below sea level. The fjord is surrounded by high mountains and the sides of the inner part of the fjord rise steeply up to above sea level. The old Dalsfjord Municipality (which existed from 1924-1964) encompassed the area surrounding this fjord. Dalsfjord Church sits on the shore of the fjord in the village of Dravlaus, just south of the mouth of the fjord. See also * List of Norwegian fjords References

{{DEFAULTSORT:Dalsfjorden (Sunnmore) Fjords of Møre og Romsdal Volda ...
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Møre Og Romsdal
Møre og Romsdal (; ) is a Counties of Norway, county in the northernmost part of Western Norway, Western Norway. It borders the counties of Trøndelag, Innlandet, and Vestland. The county administration is located in the Molde (town), town of Molde, while Ålesund (town), Ålesund is the largest town. The county is governed by the Møre og Romsdal County Municipality which includes an elected county council and a county mayor. The national government is represented by the County governor (Norway), county governor. Name The name ''Møre og Romsdal'' was created in 1936. The first element refers to the districts of Nordmøre and Sunnmøre, and the last element refers to Romsdal. Until 1919, the county was called "Romsdalens amt (subnational entity), amt", and from 1919 to 1935 "Møre fylke". For hundreds of years (1660-1919), the region was called ''Romsdalen amt (subnational entity), amt'', after the Romsdalen valley in the present-day Rauma Municipality. The Old Norse form of ...
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Norway
Norway, officially the Kingdom of Norway, is a Nordic countries, Nordic country located on the Scandinavian Peninsula in Northern Europe. The remote Arctic island of Jan Mayen and the archipelago of Svalbard also form part of the Kingdom of Norway. Bouvet Island, located in the Subantarctic, is a Dependencies of Norway, dependency, and not a part of the Kingdom; Norway also Territorial claims in Antarctica, claims the Antarctic territories of Peter I Island and Queen Maud Land. Norway has a population of 5.6 million. Its capital and largest city is Oslo. The country has a total area of . The country shares a long eastern border with Sweden, and is bordered by Finland and Russia to the northeast. Norway has an extensive coastline facing the Skagerrak strait, the North Atlantic Ocean, and the Barents Sea. The unified kingdom of Norway was established in 872 as a merger of Petty kingdoms of Norway, petty kingdoms and has existed continuously for years. From 1537 to 1814, Norway ...
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Fjord
In physical geography, a fjord (also spelled fiord in New Zealand English; ) is a long, narrow sea inlet with steep sides or cliffs, created by a glacier. Fjords exist on the coasts of Antarctica, the Arctic, and surrounding landmasses of the northern and southern hemispheres. 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 when flooded by the ocean. Thresholds above sea level create freshwater lakes. Glacial melting is accompanied by the rebounding of Earth's crust as the ice load and eroded sediment is removed (also called isostasy or gla ...
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Voldsfjorden
Voldsfjorden is a fjord in Volda Municipality in Møre og Romsdal county, Norway. The long fjord begins at the confluence of the Austefjorden and the Kilsfjorden. The Voldsfjorden reaches a maximum depth of below sea level, making it the deepest fjord in all of Sunnmøre. The fjord cuts into the mainland of Norway and it is surrounded by the Sunnmørsalpene mountains. The Dalsfjorden branches off the Voldsfjorden just south of the village of Lauvstad. The main urban area along the fjord is the village of Volda, located on the east side of the fjord. The European route E39 highway runs along the shore of part of the fjord. The fjord is crossed by two ferries going from Lauvstad to Volda, and Folkestad to Volda. See also * 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 S ...
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Norwegian Mapping Authority
The Norwegian Mapping Authority (NMA) () is Norway's national mapping agency, dealing with land surveying, geodesy Geodesy or geodetics is the science of measuring and representing the Figure of the Earth, geometry, Gravity of Earth, gravity, and Earth's rotation, spatial orientation of the Earth in Relative change, temporally varying Three-dimensional spac ..., hydrographic surveying, cadastre and cartography. The current director is Johnny Welle. Its headquarters are in Hønefoss in Ringerike Municipality. It is a public agency under the Ministry of Local Government and Regional Development. NMA was founded in 1773. The Norwegian Mapping Authority participates in research and development and cooperates with Norwegian industry and other government agencies in areas such as export-oriented measures. Tasks The NMA carries out the following tasks: *Define frameworks, methodologies and specifications for the Norwegian Spatial Data Infrastructure *Administrator and drivin ...
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Fjord
In physical geography, a fjord (also spelled fiord in New Zealand English; ) is a long, narrow sea inlet with steep sides or cliffs, created by a glacier. Fjords exist on the coasts of Antarctica, the Arctic, and surrounding landmasses of the northern and southern hemispheres. 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 when flooded by the ocean. Thresholds above sea level create freshwater lakes. Glacial melting is accompanied by the rebounding of Earth's crust as the ice load and eroded sediment is removed (also called isostasy or gla ...
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Volda Municipality
Volda is a List of municipalities of Norway, municipality in Møre og Romsdal Counties of Norway, county, Norway. It is part of the Sunnmøre Districts of Norway, region. The administrative centre is the Volda (village), village of Volda. Other villages in the municipality include Dravlaus, Fyrde, Straumshamn, Leira, Møre og Romsdal, Leira, Bjørke, and Grodås. The municipality is located about south of the town of Ålesund. The municipality is the 132nd largest by area out of the 357 municipalities in Norway. Volda Municipality is the 104th most populous municipality in Norway with a population of 11,093. The municipality's population density is and its population has increased by 9.5% over the previous 10-year period. General information The municipality of ''Volden'' was established on 1 January 1838 (see formannskapsdistrikt law). The original municipality was the same as the parish (prestegjeld) of Volden, including the sub-parishes of Ørsta Municipality, Ørsta and D ...
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Dravlaus
Dravlaus is a village in Volda Municipality in Møre og Romsdal county, Norway. The village is located along the Dalsfjorden, about south of the village of Lauvstad. The Dravlausdalen valley runs west from Dravlaus, along the Dravlauselva river. Dalsfjord Church is located in Dravlaus, along the shore of the fjord. The Dalsfjord Lighthouse Museum is located in Dravlaus. The village was the administrative centre An administrative centre is a seat of regional administration or local government, or a county town, or the place where the central administration of a commune, is located. In countries with French as the administrative language, such as Belgi ... of the old Dalsfjord Municipality which existed from 1924 until 1964. References Villages in Møre og Romsdal Volda {{MøreRomsdal-geo-stub ...
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Dalsfjord Municipality
Dalsfjord is a former municipality in Møre og Romsdal county, Norway. The municipality existed from 1924 until its dissolution in 1964. The area is now part of Volda Municipality in the traditional district of Sunnmøre. The administrative centre was the village of Dravlaus. Other villages in the municipality included Ulvestadbygda (Ulvestad, Lauvstad, and Sætre), Åmelfot, Steinsvik, and Dalsbygda. Prior to its dissolution in 1964, the municipality was the 418th largest by area out of the 689 municipalities in Norway. Dalsfjord Municipality was the 590th most populous municipality in Norway with a population of about 1,150. The municipality's population density was and its population had decreased by 0.2% over the previous 10-year period. General information Historically, the area of Dalsfjord was a part of Volda Municipality (see formannskapsdistrikt law). On 1 July 1924, the parish of Dalsfjord was separated from Volda Municipality and it was established as the new Dal ...
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Dalsfjord Church
Dalsfjord Church () is a parish church of the Church of Norway in Volda Municipality in Møre og Romsdal county, Norway. It is located in the village of Dravlaus, on the western shore of the Dalsfjorden (Sunnmøre), Dalsfjorden. It is the church for the Dalsfjord parish which is part of the Søre Sunnmøre prosti (deanery) in the Diocese of Møre. The white, wooden church was built in a Churches in Norway#Floor plan, cruciform design in 1910 using plans drawn up by the architect Ole Havnæs. The church seats about 400 people. The building was consecrated by the Bishop Johan Willoch Erichsen. History Dalsfjord did not have a church during the Middle Ages so the people of the Dalsfjord area used the main Volda Church that was located about away, on the other side of the fjord. It is said, however, that a wooden cross had been erected on the site during the Middle Ages, and that in Catholic times (pre-Reformation) this site was a gathering place for people. Sometimes the priest show ...
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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 Norway, officially the Kingdom of Norway, is a Nordic countries, Nordic country located on the Scandinavian Peninsula in Northern Europe. The remote Arctic island of Jan Mayen and the archipelago of Svalbard also form part of the Kingdom of ... Fjords ...
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Fjords Of Møre Og Romsdal
In physical geography, a fjord (also spelled fiord in New Zealand English; ) is a long, narrow sea inlet with steep sides or cliffs, created by a glacier. Fjords exist on the coasts of Antarctica, the Arctic, and surrounding landmasses of the northern and southern hemispheres. 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 when flooded by the ocean. Thresholds above sea level create freshwater lakes. Glacial melting is accompanied by the rebounding of Earth's crust as the ice load and eroded sediment is removed (also called isostasy or gla ...
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