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Raet (mango)
Raet is the largest terminal moraine in Scandinavia. It was formed during the end of the last glacial period, 12,800–11,500 years ago, in one of the latest advances of the glaciers. The moraine system extends from Finland, where it is known as Salpausselkä, through Sweden into Østfold in southeast Norway, across the Oslofjord and around the tip of southern Norway, where Raet National Park is located in Agder, then north to northern Norway and the Kola Peninsula in northwest Russia. In several regions there is more than one moraine, an older on the coast or underwater and a younger further inland. The moraines have created numerous lakes by damming watercourses, and several stretches have been used as roads since ancient times. In Norway, both Raet National Park and Jomfruland National Park are along the moraine. Formation and name The moraines were left by the retreat of the Fenno-Scandian ice sheet at the end of the Weichselian glaciation, 12,800–11,500 years ago. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arendal Tromøy Spornes B
Arendal () is a municipality in Agder county in southeastern Norway. Arendal belongs to the region of Sørlandet. The administrative centre of the municipality is the city of Arendal (which is also the seat of Agder county). Some of the notable villages in Arendal include Rykene, Eydehavn, Færvik, Strengereid, Kongshavn, Kilsund, Brattekleiv, Torsbudalen, Longum, Saltrød, Staubø, Vrengen, and Kolbjørnsvik. The offices of UNEP/GRID-Arendal are also located in the city of Arendal. The municipality is the 273rd largest by area out of the 356 municipalities in Norway. Arendal is the 23rd most populous municipality in Norway with a population of 45,509. The municipality's population density is and its population has increased by 6.3% over the previous 10-year period. General information Municipal history The town of Arendal was established as a municipality on 1 January 1838 (see formannskapsdistrikt law). On 1 January 1875, a small area with 22 inhabitants was tra ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gravel
Gravel is a loose aggregation of rock fragments. Gravel occurs naturally throughout the world as a result of sedimentary and erosive geologic processes; it is also produced in large quantities commercially as crushed stone. Gravel is classified by particle size range and includes size classes from granule- to boulder-sized fragments. In the Udden-Wentworth scale gravel is categorized into granular gravel () and pebble gravel (). ISO 14688 grades gravels as fine, medium, and coarse, with ranges 2–6.3 mm to 20–63 mm. One cubic metre of gravel typically weighs about 1,800 kg (or a cubic yard weighs about 3,000 lb). Gravel is an important commercial product, with a number of applications. Almost half of all gravel production is used as aggregate for concrete. Much of the rest is used for road construction, either in the road base or as the road surface (with or without asphalt or other binders.) Naturally occurring porous gravel deposits have a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fevik
Fevik is a Seaside resort and village in Grimstad municipality in Agder county, Norway. The village is located along the Skaggerak coast about northeast of the town of Grimstad and about south of the city of Arendal. The village of Vik lies just southwest of Fevik. The village of Fevik has a population (2015) of about 5,300 people, with most working in Arendal or central Grimstad. Since 2014, Fevik has been considered part of the "urban area" of Arendal by Statistics Norway. The European route E18 runs just to the north of the village area and the Norwegian County Road 420 runs through the village. Fevik Church is located in the village. History Fevik was a major summer tourist area from 1930 until about 1960. A large area at the northwest end of Fevik has some very interesting natural features (geological, plant, and insect) and it was made into a national nature reserve area. At the end of the 19th century, the biggest shipyard in northern Europe for iron hulls were in t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Brunlanes
Brunlanes is a parish and former municipality within Larvik municipality in Vestfold county, Norway. It was annexed by Larvik on January 1, 1988. The administrative centre of the municipality was located in the adjacent villages of Nevlunghavn and Helgeroa. Arguably the best soil in Vestfold County can be found in Brunlanes, and farming is the main industry with considerable vegetable- and corn cultivation. It is home to Berg Old Church at Berg, which was erected in the 1100s, but laid in ruins by the 1960s. The church had been rebuilt and features a clear-cut architecture with a red tilestone roof. History The parish of Brunlagnæs was established as a municipality January 1, 1838 (see formannskapsdistrikt). Small parts of Brunlanes were moved to Larvik in 1875 and to the neighboring municipality Stavern in 1883, 1938, 1949 and 1969. In 1964 three farms with 12 inhabitants were moved to Porsgrunn in Telemark county. On 1 January 1988 Brunlanes was incorporated into the enlarge ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
European Route E18
European route E18 runs from Craigavon in Northern Ireland to Saint Petersburg in Russia, passing through Scotland, England, Norway, Sweden and Finland. It is about in length. Although the designation implies the possibility of a through journey, this is no longer practical as there are no direct car ferry crossings between the United Kingdom and Norway. United Kingdom The route starts in Northern Ireland and runs from Craigavon ( M1) – Belfast ( M2, A8) – Larne, then to Scotland: Stranraer, Dumfries and Galloway ( A75) – Gretna – then England via the ( M6) – Carlisle ( A69) to Newcastle. As is normal for European routes in the United Kingdom, it is not signposted as such. Northern Ireland *: Craigavon - Belfast (Start of multiplex with at Lisburn) *: Belfast *: Belfast - (Multiplex with ) *: - *: - Larne (End of multiplex with ) North Channel *: Larne - Cairnryan Great Britain *: Stranraer - *: - ''Anglo-Scottish border'' (Start of multiplex w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vestfold
Vestfold is a traditional region, a former county and a current electoral district in Eastern Norway. In 2020 the county became part of the much larger county of Vestfold og Telemark. Located on the western shore of the Oslofjord, it bordered the previous Buskerud and Telemark counties. The county administration was located in Tønsberg, Norway's oldest city, and the largest city is Sandefjord. With the exception of the city-county of Oslo, Vestfold was the smallest county in Norway by area. Vestfold was the only county in which all municipalities had declared Bokmål to be their sole official written form of the Norwegian language. Vestfold is located west of the Oslofjord, as the name indicates. It includes many smaller, but well-known towns in Norway, such as Larvik, Sandefjord, Tønsberg and Horten; these towns run from Oslo in an almost constant belt of urban areas along the coast, ending in Grenland in neighbouring region Telemark. The river Numedalslågen runs through th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Moss, Norway
is a coastal town and a municipality in Viken county, Norway. The administrative centre of the municipality is the town of Moss. The city of Moss was established as a municipality on 1 January 1838 (see formannskapsdistrikt) and City in 1720. The rural municipality of Jeløy was merged with the city on 1 July 1943. The former municipality of Rygge was merged into it on January 1, 2020. Its administrative district covers areas east of the town, such as the island of Dillingøy in the lake Vansjø. Parts of the town are located on the peninsula of Jeløy. The city of Moss has 30,723 inhabitants (2012). Name The Old Norse form of the name was . It may be derived from an old root ''mer-'' which means to "divide" or "split". The adjacent topography shares similar etymology: * , Mosse-"marsh-river-border"+ (see , , Old Norse for river). The name is thought to be very old and the meaning of it is not clear. * , Mosse-"marsh-river-border"+ (Moss channel). * , Mosse-"marsh-river-bo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Halden
Halden (), between 1665 and 1928 known as Fredrikshald, is both a town and a municipality in Viken county, Norway. The municipality borders Sarpsborg to the northwest, Rakkestad to the north and Aremark to the east, as well as the Swedish municipalities Strömstad, Tanum and Dals-Ed respectively to the southwest, south and southeast. The seat of the municipality, Halden is a border town located at the mouth of the Tista river on the Iddefjord, the southernmost border crossing between Norway and Sweden. The town of Halden is located about south of Oslo, north of Gothenburg, and east of the border crossing at Svinesund Bridge, Svinesund. History Evidence of early human settlements in this region of Norway have been found, particularly in the Svinesund area of the municipality where evidence of early settlements from the Nordic Bronze Age have been found. Named after a small farm ''Hallen'' ( en, "rise" or "slope") first mentioned in 1629, "Halden", became the city of ''Fred ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vänern
Vänern ( , also , ) is the largest lake in Sweden, the largest lake in the European Union and the third-largest lake of all Europe after Ladoga and Onega in Russia. It is located in the provinces of Västergötland, Dalsland, and Värmland in the southwest of the country. With its surface located at with a maximum depth of , the lowest point of the Vänern basin is at below sea level. The average depth is at a more modest , which means that the average point of the lake floor remains above sea level. Vänern drains into Göta älv towards Gothenburg and the Kattegat tributary of the Atlantic Ocean. It is the only one of the ten largest lakes in Sweden not to drain on the country's eastern coastline. Due to the construction of Göta Canal in the 19th century, there is an upstream water path to Vättern and the east coast from Vänern. The main inflow of water comes from Klarälven entering Vänern near Karlstad with its source in Trøndelag in Norway. History The southeas ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Central Swedish Ice-edge Zone
The central Swedish ice-edge zone was formed when the melting of inland ice slowed during a cold period approximately 12,000 years ago and the ice edge stood relatively still for around 800 years. This occurred during the Younger Dryas period. The two main terminal moraines of this zone are the Skövde and Billigen ones. These two terminal moraines form parallel and semicontinuous ridges spanning from the Västgöta plains though the Östgöta plains to the Stockholm archipelago. See also *Central Swedish lowland The Central Swedish lowland ( sv, Mellansvenska sänkan, Mellansvenska låglandet) is a large region of low relief and altitude in Sweden spanning from the Swedish West Coast at Bohuslän to Stockholm archipelago and Roslagen at the Baltic Sea. T ... References {{reflist Geology of Sweden Geography of Sweden Glacial deposits of Sweden Moraines of Europe Pleistocene Europe Pleistocene geology ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
