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Kodal Kirke
Kodal is a village and parish in Sandefjord municipality in Vestfold county, Norway. Kodal is mostly a rural area, with a population of 971 as of 2014. It is located ten kilometers north of Sandefjord city center and eleven miles south of the town center in Andebu. Kodal has one gas station, an elementary school, a kindergarten, grocery store, sports center, church, and two traffic schools. Several burial mounds dating back to the Viking Age have been found in the area. Kodal Church (''Kodal kirke'') is located in Prestbøen. Agriculture is an important industry in Kodal, but large amounts of iron and phosphorus also occur. The amount of granite is estimated to be 100 million tons. Etymology Previous written forms of the name were Kvodal (from 1376), Kuadal (1390), Quadal (1414), and Quodal (1558). Its current spelling ''Kodal'' is kept from the 17th century. The first portion of the name, Ko-, may refer to the smaller river now known as Ivjua, which was formerly known as Kvaða/ ...
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Kodal Kirke
Kodal is a village and parish in Sandefjord municipality in Vestfold county, Norway. Kodal is mostly a rural area, with a population of 971 as of 2014. It is located ten kilometers north of Sandefjord city center and eleven miles south of the town center in Andebu. Kodal has one gas station, an elementary school, a kindergarten, grocery store, sports center, church, and two traffic schools. Several burial mounds dating back to the Viking Age have been found in the area. Kodal Church (''Kodal kirke'') is located in Prestbøen. Agriculture is an important industry in Kodal, but large amounts of iron and phosphorus also occur. The amount of granite is estimated to be 100 million tons. Etymology Previous written forms of the name were Kvodal (from 1376), Kuadal (1390), Quadal (1414), and Quodal (1558). Its current spelling ''Kodal'' is kept from the 17th century. The first portion of the name, Ko-, may refer to the smaller river now known as Ivjua, which was formerly known as Kvaða/ ...
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Sandefjord
Sandefjord () is a city and the most populous municipality in Vestfold og Telemark county, Norway. The municipality of Sandefjord was established on 1 January 1838. The municipality of Sandar was merged into Sandefjord on 1 January 1969. On 1 January 2017, rural municipalities of Andebu and Stokke were merged into Sandefjord as part of a nationwide municipal reform. This merger was the first one to take place during the reform. The city is known for its rich Viking history and the prosperous whaling industry, which made Sandefjord the richest city in Norway.Porter, Darwin and Danforth Prince (2003). ''Frommer's Norway''. Wiley. p. 158. . Today, it has built up the third-largest merchant fleet in Norway. It is home to Europe's only museum dedicated to whaling, and is home to Gokstad Mound where the 9th century Gokstad Ship was discovered. Sandefjord has numerous nicknames, including the Viking, Whaling "capital" of Norway or as the undisputed summer city of Norway. The city i ...
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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 ...
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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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Andebu
Andebu is a village in Sandefjord municipality, Vestfold County, and a former municipality. The administrative centre of the municipality was the village of Andebu. The village is surrounded by forests, mountains, and hills. Its nearest cities are Sandefjord and Tønsberg. The parish of ''Andebo'' was established as a municipality on 1 January 1838 (see formannskapsdistrikt). On 1 January 2017, the municipality became a part of Sandefjord municipality, along with Stokke. The former municipality now makes up the northernmost part of Sandefjord municipality. Andebu was the fourth-largest municipality in Vestfold and is situated in the center of the county. Its economy is primarily related to logging and forestry. Andebu has been inhabited for centuries and the oldest artifacts retrieved here dates back 4000 years to the Iron Age. Most retrieved artifacts are various types of tools, mainly axes made of flint and other rocks. Andebu’s geography consists mainly of valleys, hills, m ...
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Viking Age
The Viking Age () was the period during the Middle Ages when Norsemen known as Vikings undertook large-scale raiding, colonizing, conquest, and trading throughout Europe and reached North America. It followed the Migration Period and the Germanic Iron Age. The Viking Age applies not only to their homeland of Scandinavia but also to any place significantly settled by Scandinavians during the period. The Scandinavians of the Viking Age are often referred to as ''Vikings'' as well as ''Norsemen'', although few of them were Vikings in sense of being engaged in piracy. Voyaging by sea from their homelands in Denmark, Norway, and Sweden, the Norse people settled in the British Isles, Ireland, the Faroe Islands, Iceland, Greenland, Normandy, and the Baltic coast and along the Dnieper and Volga trade routes in eastern Europe, where they were also known as Varangians. They also briefly settled in Newfoundland, becoming the first Europeans to reach North America. The Norse-Gaels, ...
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Kodal Church
Kodal Church ( no, Kodal kirke) is a long church ( no, langkirke) located in Kodal in the municipality of Sandefjord in Vestfold og Telemark county, Norway. The church is the parish church for Kodal. Its chancel dates from the 12th century. The nave dates from 1691 and is made of round timbers. The altarpiece dates from 1781, and the painting ''Jesus and the Disciples on the Walk to Emmaus'' by Otto Valstad is painted in the style of Anton Dorph and is from 1899. Kodal Church was mentioned in written sources for the first time in 1339. When the medieval Sandar Church, located about south of Kodal Church, was razed in 1790, the altarpiece from Sandar was moved to Kodal Church. In 1893 Kodal Church received its first organ, and in 1919 new bells from the Olsen Nauen Bell Foundry The Olsen Nauen Bell Foundry ( no, Olsen Nauen Klokkestøperi) is a Norwegian bell foundry located in the municipality of Tønsberg. The foundry was established in 1844 by Ole Olsen, and it is head ...
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Iron
Iron () is a chemical element with symbol Fe (from la, ferrum) and atomic number 26. It is a metal that belongs to the first transition series and group 8 of the periodic table. It is, by mass, the most common element on Earth, right in front of oxygen (32.1% and 30.1%, respectively), forming much of Earth's outer and inner core. It is the fourth most common element in the Earth's crust. In its metallic state, iron is rare in the Earth's crust, limited mainly to deposition by meteorites. Iron ores, by contrast, are among the most abundant in the Earth's crust, although extracting usable metal from them requires kilns or furnaces capable of reaching or higher, about higher than that required to smelt copper. Humans started to master that process in Eurasia during the 2nd millennium BCE and the use of iron tools and weapons began to displace copper alloys, in some regions, only around 1200 BCE. That event is considered the transition from the Bronze Age to the Iron A ...
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Phosphorus
Phosphorus is a chemical element with the symbol P and atomic number 15. Elemental phosphorus exists in two major forms, white phosphorus and red phosphorus, but because it is highly reactive, phosphorus is never found as a free element on Earth. It has a concentration in the Earth's crust of about one gram per kilogram (compare copper at about 0.06 grams). In minerals, phosphorus generally occurs as phosphate. Elemental phosphorus was first isolated as white phosphorus in 1669. White phosphorus emits a faint glow when exposed to oxygen – hence the name, taken from Greek mythology, meaning 'light-bearer' (Latin ), referring to the " Morning Star", the planet Venus. The term '' phosphorescence'', meaning glow after illumination, derives from this property of phosphorus, although the word has since been used for a different physical process that produces a glow. The glow of phosphorus is caused by oxidation of the white (but not red) phosphorus — a process now called chem ...
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Granite
Granite () is a coarse-grained (phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or ''granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) contain almost no dark minerals. Granite is nearly alway ...
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