Slependen
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Slependen
Slependen is a relatively large area in Bærum, Norway. On Slependen there is significant villa settlement, as well as considerable office and commercial activities. Building development Slependen posed originally as an area across large parts of Asker and Bærum. In 1927 the area was split due to the different priorities of the two municipalities in terms of financial support. The area that belonged to Bærum, where the two larger farms Gyssestad and Hilton held to, was given the name ''Øvre Slependen Vel'' (Upper Slependen Well area). Gyssestad farm was bought and taken over by the municipality of Bærum in 1950, but is today completely downsized. The original municipal boundary was a stream of Åsløkka in Hilton hill that ran out in Slependbukta. Road construction in the area has taken a lot of the earth and residential construction started early. A popular area is Åsløkkveien, from where there are views of Oslofjorden. After one of the stations on the Drammen Line was na ...
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Slependen Station
Slependen Station ( no, Slependen holdeplass) is a railway station on the Drammen Line located at Slependen in Bærum, Norway. Situated from Oslo Central Station, it consists of an island platform and serves the L1 line of the Oslo Commuter Rail operated by the Norwegian State Railways. It had 900 daily passengers in 2008. The first station at Slependen was located further west and opened on 11 September 1873, a year after the Drammen Line. It was variously known as Slæbenden and Slæbende until it took its present name in 1921. A new station building was erected in 1916 and demolished in 1960. With the doubling of the Drammen Line, Slependen was rebuilt to the east, still on a curve, as an elevated station. This station was designed by Ina Backer. That station and the one to the east, Jong Station, were closed on 23 May 1993 and replaced by the current station, designed by Arne Henriksen. History The Drammen Line through Slependen opened as a narrow gauge railway on 7 Oct ...
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Bærum
Bærum () is a municipality in the Greater Oslo Region in Norway that forms an affluent suburb of Oslo on the west coast of the city. Bærum is Norway's fifth largest municipality with a population of 128,760 (2021). It is part of the electoral district and historical county of Akershus and of the newer Viken County. The administrative centre of the municipality is the town of Sandvika. Bærum was established as a municipality on 1 January 1838. Bærum has the highest income per capita in Norway and the highest proportion of university-educated individuals. Bærum, particularly its eastern neighbourhoods bordering West End Oslo, is one of Norway's priciest and most fashionable residential areas, leading Bærum residents to be frequently stereotyped as snobs in Norwegian popular culture. The municipality has been voted the best Norwegian place to live in considering governance and public services to citizens. Name The name (Old Norse: ''Bergheimr'') is composed of ''berg'', whi ...
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Asker
Asker ( no, Asker), properly called Askerbygda in Norwegian, is a district and former Municipalities of Norway, municipality in Akershus, Norway. From 2020 it is part of the larger administrative municipality Asker, Viken (also known as Greater Asker) in Viken (county), Viken county, together with the traditional Buskerud districts Røyken and Hurum; Asker proper constitutes the northern fourth and is part of the Greater Oslo Region. The administrative centre was the town of Asker, which remains so for the new larger municipality. Asker was established as a parish in the Middle Ages and as a municipality Formannskapsdistrikt, on 1 January 1838. History Since the Middle Ages, the Asker parish consisted of the later municipalities Asker and Bærum. In the 19th century Bærum became the Vestre Bærum and Østre Bærum parish, and Asker and Bærum were also established as separate municipalities. In 2020, Asker municipality merged with Røyken and Hurum to form Asker, Viken, a la ...
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Akershus
Akershus () is a traditional region and current electoral district in Norway, with Oslo as its main city and traditional capital. It is named after the Akershus Fortress in Oslo. From the middle ages to 1919, Akershus was a fief and main county that included most of Eastern Norway, and from the 17th century until 2020, Akershus also had a more narrow meaning as a (sub) county that included most of the Greater Oslo Region. After 2020 the former county of Akershus was merged into Viken along with the former counties of Østfold and Buskerud. In 2022 the Storting voted to dissolve Viken and reestablish Akershus county. Originally Akershus was one of four main fiefs in Norway and included almost all of Eastern Norway. The original Akershus became a main county (''Stiftamt'' or ''Stift'') in 1662 and was sometimes also known as ''Christiania Stift''. It included several subcounties (''Amt'' or ''Underamt''); in 1682 its most central areas, consisting of modern Oslo and Akershus, beca ...
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Calcination
Calcination refers to thermal treatment of a solid chemical compound (e.g. mixed carbonate ores) whereby the compound is raised to high temperature without melting under restricted supply of ambient oxygen (i.e. gaseous O2 fraction of air), generally for the purpose of removing impurities or volatile substances and/or to incur thermal decomposition. The root of the word calcination refers to its most prominent use, which is to remove carbon from limestone (calcium carbonate) through combustion to yield calcium oxide (quicklime). This calcination reaction is CaCO3(s) → CaO(s) + CO2(g). Calcium oxide is a crucial ingredient in modern cement, and is also used as a chemical flux in smelting. Industrial calcination generally emits carbon dioxide (), making it a major contributor to climate change. A calciner is a steel cylinder that rotates inside a heated furnace and performs indirect high-temperature processing (550–1150 °C, or 1000–2100 °F) within a controlled ...
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Cities And Towns In Norway
A city is a human settlement of notable size.Goodall, B. (1987) ''The Penguin Dictionary of Human Geography''. London: Penguin.Kuper, A. and Kuper, J., eds (1996) ''The Social Science Encyclopedia''. 2nd edition. London: Routledge. It can be defined as a permanent and densely settled place with administratively defined boundaries whose members work primarily on non-agricultural tasks. Cities generally have extensive systems for housing, transportation, sanitation, utilities, land use, production of goods, and communication. Their density facilitates interaction between people, government organisations and businesses, sometimes benefiting different parties in the process, such as improving efficiency of goods and service distribution. Historically, city-dwellers have been a small proportion of humanity overall, but following two centuries of unprecedented and rapid urbanization, more than half of the world population now lives in cities, which has had profound consequences for g ...
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Akershus Fortress
Akershus Fortress ( no, Akershus Festning, ) or Akershus Castle ( no, Akershus slott ) is a medieval castle in the Norwegian capital Oslo that was built to protect and provide a royal residence for the city. Since the Middle Ages the fortress has been the namesake and centre of the main fief and later main county of Akershus, which was originally one of Norway's four main regions and which included most of Eastern Norway. The fortress itself was located within the Akershus main county until 1919, and also within the smaller Akershus sub county until 1842. The castle has also been used as a military base, a prison and is currently the temporary office of the Prime minister of Norway. Construction It is not known exactly when the construction of the castle started but it is believed that it took place around the late 1290s, by King Haakon V, replacing Tønsberg as one of the two most important Norwegian castles of the period (the other being Båhus). It was constructed in ...
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Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ...
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