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Húnavatnshreppur
Húnavatnshreppur () is a former rural municipality located in northwestern Iceland. History The municipality was formed on 1 January 2006 by the union of the former municipalities of Sveinsstaðahreppur , Torfalækjarhreppur , Svínavatnshreppur and Bólstaðarhlíðarhreppur . In 2022, the municipality merged with Blönduós to form Húnabyggð. Geography Húnavatn is one of the largest Icelandic municipalities. Its southern borders touch the glaciers of Hofsjökull and Langjökull. In the south are situated also the hot springs in Hveravellir Hveravellir () is a geothermal field (high temperature field) of the Oddnýjarhnjúkur-Langjökull subglacial volcanic system in the north of Langjökull glacier. Description Hveravellir geothermal area is a small nature reserve and a tourist .... References External links Official website Former municipalities of Iceland Northwestern Region (Iceland) States and territories disestablished in 2022 {{Iceland ...
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Húnabyggð
Húnabyggð is a municipality in the north of Iceland, which was formed with the merger of Blönduós and Húnavatnshreppur. An vote was held in February 2022 where 97.8% of Blönduós inhabitants and 62.3% of Húnavatnshreppur inhabitants voted with the merge. The merger was finalized in the municipality elections in March 2022. Húnabyggð is among the largest municipalities of Iceland in terms of area and reaches from Húnaflói, where Blönduós is situated, to the interior, where Langjökull and Hofsjökull __NOTOC__ Hofsjökull ( Icelandic: "temple glacier", ) is the third largest ice cap in Iceland after Vatnajökull and Langjökull and the largest active volcano in the country. It is situated in the west of the Highlands of Iceland and north of ... are situated. Blönduvirkjun hydropower plant is situated in the municipality. References Municipalities of Iceland Populated places in Northwestern Region (Iceland) States and territories established in 2022 { ...
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Blönduós
Blönduós () is a town and former municipality in the north of Iceland with a population of 895 in 2018. Like many towns and villages around Iceland, Blönduós did not emerge as a village until the late 19th century. The town is situated on Route 1 at the mouth of the glacial river Blanda. Hrútey , a small island and natural reserve encircled by the river, is accessible via a pedestrian bridge just off the ring road. In 2022, the town merged with Húnavatnshreppur to form Húnabyggð. Geography One of Blönduós' main characteristics is that the town is split into two parts by the glacial river Blanda, for which it is named (Blöndu is an oblique case of Blanda). The old part of town ( Icelandic: "gamli bærinn"), including many original houses from the late 19th and early 20th century, is located on the south side of the river. Many of the local companies, the elementary school, supermarket, community center and sports facilities including a modern outdoor heated pool are ...
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Hveravellir
Hveravellir () is a geothermal field (high temperature field) of the Oddnýjarhnjúkur-Langjökull subglacial volcanic system in the north of Langjökull glacier. Description Hveravellir geothermal area is a small nature reserve and a tourist centre located in 600 m a.s.l. at the Kjölur mountain route between the glaciers Hofsjökull and Langjökull, Central Iceland. It is part of the Oddnýjarhnjúkur-Langjökull volcanic system. The place has been a popular resting place in highland travels since the age of settlement, 1100-1200 years ago. It is frequently mentioned in the old sagas, annals and folklore. Refuge huts have been situated there from the early beginning. The main geothermal activity is at the northern border of the large lava shield Kjalhraun . The main geothermal area covers around 2.5 km². The hot springs are of various types, geysers, fumaroles, solfataras, boiling pits and warm springs with lower temperatures. The currently active geysers only have smal ...
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Northwest Constituency
Northwest ( is, Norðvestur) is one of the six multi-member constituencies of the Althing, the national legislature of Iceland. The constituency was established as Northwestern ( is, Norðurland vestra ) in 1959 following the nationwide extension of proportional representation for elections to the Althing. It was renamed Northwest in 2003 when the Western and Westfjords constituencies were merged into the Northwestern constituency following the re-organisation of constituencies across Iceland. Northwest consists of the regions of Northwestern, Western and Westfjords. The constituency currently elects seven of the 63 members of the Althing using the open party-list proportional representation electoral system. At the 2021 parliamentary election it had 21,541 registered electors. Electoral system Northwest currently elects seven of the 63 members of the Althing using the open party-list proportional representation electoral system. Constituency seats are allocated using the D'Ho ...
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Regions Of Iceland
The regions of Iceland are eight areas of Iceland that roughly follow the arrangement of parliamentary constituencies as they were between 1959 and 2003. These regions are not incorporated polities but rather recognized groupings of municipalities. Iceland only has two levels of administration, the national government and 69 municipalities. The municipalities have organized themselves into eight regional associations and those boundaries are also recognized by Statistics Iceland to report statistics. Since 2014, police and commissioner (''sýslumaður'') districts have followed the eight region model with the exception that Vestmannaeyjar form a special district and are not part of the South region. The divisions of Iceland for the purposes of health care and district courts diverge more from the commonly used eight region model. The postal code system also roughly corresponds with the regions with the first digit of the three digit codes usually being the same as on the map below ...
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Hot Spring
A hot spring, hydrothermal spring, or geothermal spring is a spring produced by the emergence of geothermally heated groundwater onto the surface of the Earth. The groundwater is heated either by shallow bodies of magma (molten rock) or by circulation through faults to hot rock deep in the Earth's crust. In either case, the ultimate source of the heat is radioactive decay of naturally occurring radioactive elements in the Earth's mantle, the layer beneath the crust. Hot spring water often contains large amounts of dissolved minerals. The chemistry of hot springs ranges from acid sulfate springs with a pH as low as 0.8, to alkaline chloride springs saturated with silica, to bicarbonate springs saturated with carbon dioxide and carbonate minerals. Some springs also contain abundant dissolved iron. The minerals brought to the surface in hot springs often feed communities of extremophiles, microorganisms adapted to extreme conditions, and it is possible that life on Earth had its ...
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Langjökull
Langjökull (, Icelandic for "long glacier") is the second largest ice cap in Iceland (953 km2), after Vatnajökull. It is situated in the west of the Icelandic interior or Highlands of Iceland and can be seen clearly from Haukadalur. Its volume is 195 km³ and the ice is up to thick. The highest point of the ice cap (at ''Baldjökull'' at the northern end of Langjökull) is about above sea level. In the past, the largest recorded surface area was in 1840. Situation and form The glacier is roughly parallel to the direction of the country's active volcanic zone: north-east to south-west. It is about long and wide, and has a slightly narrower point roughly between the lake Hvítárvatn on the Kjölur mountain road to the east and the Þrístapajökull glacier to the west, near another smaller glacier, Eiríksjökull, which is not quite connected to Langjökull. It is the nearest large glacier to Reykjavík. The area of the glacier includes some mountains, e.g. ...
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Hofsjökull
__NOTOC__ Hofsjökull ( Icelandic: "temple glacier", ) is the third largest ice cap in Iceland after Vatnajökull and Langjökull and the largest active volcano in the country. It is situated in the west of the Highlands of Iceland and north of the mountain range Kerlingarfjöll, between the two largest glaciers of Iceland. It covers an area of 925 km2, reaching at its summit. The subglacial volcano is a shield type with caldera. Hofsjökull is the source of several rivers including the Þjórsá, Iceland's longest river. In the southeast of Iceland, between the easternmost glacier tongue of Vatnajökull (Axajökull) and Þrándarjökull, there is a smaller glacier (area about 4 km2), which is also called Hofsjökull. In 2015, Hofsjökull increased in mass, the first time in 20 years this had happened. See also * Glaciers of Iceland * Iceland plume * List of volcanoes in Iceland Notes References * External links Hofsjökullin the Catalogue of Icelandic Volcano ...
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Glaciers Of Iceland
The glaciers and ice caps of Iceland cover 11% of the land area of the country (about 11,400 km² out of the total area of 103,125 km²) and have a considerable impact on its landscape and meteorology. Glaciers are also contributing to the Icelandic economy, with tourists flocking to the country to see glaciers on snowmobiles and on glacier hiking tours. However, the recent loss of ice due to climate change is an increasing concern in Icelandic society. Description An ice cap is a mass of glacial ice that covers less than 50,000 km² of land area covering a highland area and they feed outlet glaciers. Many Icelandic ice caps and glaciers lie above volcanoes, such as Grímsvötn and Bárðarbunga, which lie under the largest ice cap, Vatnajökull. The caldera of Grímsvötn is 100 km² in area, and Bárðarbunga is 60 km². When volcanic activity occurs under the glacier, the resulting meltwater can lead to a sudden glacial lake outburst flood, known in ...
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Northwestern Region (Iceland)
Northwestern Region ( is, Norðurland vestra ) is one of the traditional eight regions of Iceland, located in the north of the island. The largest town in the region is Sauðárkrókur, with a population of 3000. One of the primary attractions of the area is the basalt rock Hvítserkur (, regionally also ) is a 15 m high basalt Stack (geology), stack along the eastern shore of the Vatnsnes peninsula, in Northwestern Region (Iceland), northwest Iceland. The rock has two holes at the base, which give it the appearance of a ..., 15 meters high and resembles a dragon that throws its head to take a sip of water. References External links * {{iceland-geo-stub ...
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