List Of Mountains In Iceland
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List Of Mountains In Iceland
* Hekla (1,491 m), Iceland, volcano * Öræfajökull (2,110 m), Iceland, volcano - highest mountain in Iceland * Snæfellsjökull (1,448 m), Iceland, volcano * Esjan (914 m), Iceland, -about 10 km north of Reykjavík {{List of mountains in Europe Iceland Mountains Iceland Iceland ( is, Ísland; ) is a Nordic island country in the North Atlantic Ocean and in the Arctic Ocean. Iceland is the most sparsely populated country in Europe. Iceland's capital and largest city is Reykjavík, which (along with its s ...
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Hekla
Hekla (), or Hecla, is a stratovolcano in the south of Iceland with a height of . Hekla is one of Iceland's most active volcanoes; over 20 eruptions have occurred in and around the volcano since 874. During the Middle Ages, the Icelandic Norse called the volcano the "Gateway to Hell". Hekla is part of a volcanic ridge, long. The most active part of this ridge, a fissure about long named , is considered to be within Hekla proper. Hekla looks rather like an overturned boat, with its keel being a series of craters, two of which are generally the most active. The volcano's frequent large eruptions have covered much of Iceland with tephra, and these layers can be used to date eruptions of Iceland's other volcanoes. Approximately 10% of the tephra created in Iceland in the last thousand years has come from Hekla, amounting to 5 km3. Cumulatively, the volcano has produced one of the largest volumes of lava of any in the world in the last millennium, around 8 km3. Etymolo ...
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Herðubreið
Herðubreið (, ''broad-shouldered'') is a tuya in northern part of Vatnajökull National Park, Iceland. It is situated in the Highlands of Iceland at the east side of the Ódáðahraun desert and close to Askja volcano. The desert is a large lava field originating from eruptions of Trölladyngja and other shield volcanoes in the area. Herðubreið was formed beneath the icesheet that covered Iceland during the last glacial period. Overview Due to the mountain's steep and unstable sides, the first ascent was in 1908 despite centuries of knowledge of its existence. The Mountain is often referred to as "The Queen of Icelandic Mountains" by Icelanders due to its beautiful shape. Near the mountain lies an oasis called Herðubreiðarlindir with a campground and hiking trails. In former times, outcasts who had been excluded from Icelandic society because of crimes they had committed lived at the oasis. One such outlaw was Fjalla-Eyvindur, who lived there during the winter of 177 ...
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Lists Of Mountains By Country
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Mountains Of Iceland
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited Summit (topography), summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are Monadnock, isolated summits, but most occur in mountain ranges. Mountain formation, Mountains are formed through Tectonic plate, tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosys ...
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Kerling (Iceland)
Mount Kerling (, "Old Hag") is the highest mountain (1538 m) in the District of Eyjafjarðarsveit, in the northern part of Iceland. Its structure is mainly basaltic rock, but the uppermost part is rhyolite, which extends to Mts Súlur nearby and all the way to the lower slopes of Mt. Vindheimajökull to the north of valley Glerá The Glerá (, "glass river") is a river in northern Iceland. It originates from glaciers in the mountains of the Tröllaskagi peninsula and also draws from some freshwater springs on its way down Glerá Valley. It runs through the town of Akur ...rdalur. It is considered an easy climb with excellent panoramic views on a fine day. References Mountains of Iceland One-thousanders of Iceland {{Iceland-geo-stub ...
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Tungnafellsjökull
Tungnafellsjökull (, "''Tungna-fells glacier''" or "tongue-fells glacier") is a glacier and volcano in Iceland. It has an elevation of and is located northwest of Vatnajökull glacier. ReferencesVolcano Discovery External links Tungnafellsjökullin the Catalogue of Icelandic Volcanoes Catalog or catalogue may refer to: *Cataloging **'emmy on the 'og **in science and technology *** Library catalog, a catalog of books and other media ****Union catalog, a combined library catalog describing the collections of a number of librarie ... * Glaciers of Iceland Volcanoes of Iceland Mid-Iceland Belt Subglacial volcanoes of Iceland {{Iceland-glacier-stub ...
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Eyjafjallajökull
Eyjafjallajökull (; ), sometimes referred to by the numeronym E15, is one of the smaller ice caps of Iceland, north of Skógar and west of Mýrdalsjökull. The ice cap covers the caldera of a volcano with a summit elevation of . The volcano has erupted relatively frequently since the Last Glacial Period, most recently in 2010, when, although relatively small for a volcanic eruption, it caused enormous disruption to air travel across northern and western Europe for a week. Geography Eyjafjallajökull consists of a volcano completely covered by an ice cap. The ice cap covers an area of about , feeding many outlet glaciers. The main outlet glaciers are to the north: Gígjökull , flowing into Lónið , and Steinholtsjökull , flowing into Steinholtslón . In 1967, there was a massive landslide on the Steinholtsjökull glacial tongue. On 16 January 1967 at 13:47:55 there was an explosion on the glacier. It can be timed because the seismometers at Kirkjubæjarklaustur monitor ...
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Eiríksjökull
Eiríksjökull ( Icelandic for "Eirík's glacier", ) is a glacier north-west of Langjökull in Iceland, with an area of reaching a height of , making it the largest table mountain in Iceland. Rising over above its surrounding, the lowest of a hyaloclastite (móberg) tuya formed presumably by a single subglacial volcanic activity is capped by a thick lava shield A shield volcano is a type of volcano named for its low profile, resembling a warrior's shield lying on the ground. It is formed by the eruption of highly fluid (low viscosity) lava, which travels farther and forms thinner flows than the mo .... It is currently dormant or extinct in terms of volcanic activity. Etymology The glacier was called Baldjökull until about 1700 and with relative certainty the current name is influenced by the nearby mountain Eiríksgnípa. Nothing is known with certainty about said Erik but a fable tells of an outlaw named Eiríkur or Eirekur who evaded capture by running into that m ...
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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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Iceland
Iceland ( is, Ísland; ) is a Nordic island country in the North Atlantic Ocean and in the Arctic Ocean. Iceland is the most sparsely populated country in Europe. Iceland's capital and largest city is Reykjavík, which (along with its surrounding areas) is home to over 65% of the population. Iceland is the biggest part of the Mid-Atlantic Ridge that rises above sea level, and its central volcanic plateau is erupting almost constantly. The interior consists of a plateau characterised by sand and lava fields, mountains, and glaciers, and many glacial rivers flow to the sea through the lowlands. Iceland is warmed by the Gulf Stream and has a temperate climate, despite a high latitude just outside the Arctic Circle. Its high latitude and marine influence keep summers chilly, and most of its islands have a polar climate. According to the ancient manuscript , the settlement of Iceland began in 874 AD when the Norwegian chieftain Ingólfr Arnarson became the first p ...
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Kverkfjöll
Kverkfjöll (; 1,764 m) is a mountain range situated on the north-eastern border of the glacier Vatnajökull in Iceland. With the glacier Kverkjökull, it is between the Vatnajökull glacier and the Dyngjufjöll mountains. The mountains are active volcanoes. Especially around 1720, they saw frequent eruptions and glacier runs. Under the mountains, there is a magma chamber which leads to the formation of glacier caves. Currently, they cannot be visited because of the risk of collapse. The Holuhraun lava field is approximately to the north-west of Kverkfjöll. The main volume of the Jökulsá á Fjöllum river flows from the Kverkfjöll area. See also * Glaciers of Iceland * Iceland plume * List of lakes of Iceland * List of volcanoes in Iceland * Volcanism of Iceland External links Kverksfjöllin the Catalogue of Icelandic Volcanoes Catalog or catalogue may refer to: *Cataloging **'emmy on the 'og **in science and technology *** Library catalog, a catalog of books and ot ...
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Bárðarbunga
Bárðarbunga (), is a stratovolcano located under Vatnajökull in Vatnajökull National Park which is Iceland's most extensive glacier. The second highest mountain in Iceland, above sea level, Bárðarbunga is also part of a volcanic system that is approximately long and wide. Description Bárðarbunga is a subglacial stratovolcano under the ice cap of Vatnajökull glacier in the Vatnajökull National Park in Iceland. It rises to above sea level, making it the second highest mountain in Iceland, about lower than Hvannadalshnjúkur. The caldera is about 80 square kilometres, up to 10 km wide and about deep. The surrounding edges rise to 1,850 metres, but the base is on average close to 1,100 metres. The volcano is covered in ice to a depth of 850m, hiding the glacier-filled crater. The associated volcanic system and fissure swarm is about 190 km long and 25 km wide. Bárðarbunga was a little-known volcano in Iceland due to its remote location and infrequ ...
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