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List Of Volcanoes In Iceland
This list of volcanoes in Iceland includes active and dormant volcanic mountains, of which 18 have erupted since human settlement of Iceland began around 900 AD. __TOC__ List Volcanic zones and systems Iceland has four major volcanic zones surrounding an hypothetical hotspot: * the Reykjanes zone (RVZ), subdivided into the Reykjanes Ridge (RR) (the Mid-Atlantic Ridge South of Iceland) and the Reykjanes Volcanic Belt (RVB) (on the main island); * the West Volcanic Zone (WVZ); * the East Volcanic Zone (EVZ) (extended to the Westman Islands, South of the main island); * the North Volcanic Zone (NVZ). The Mid-Iceland Belt (MIB) connects them across central Iceland. In Iceland's East Volcanic Zone (EVZ), the central volcanoes, Vonarskarð and Hágöngur belong to the same volcanic system; this also applies to Bárðarbunga and Hamarinn, and to Grímsvötn and Þórðarhyrna. North of Iceland, the Mid-Atlantic Ridge is called Kolbeinsey Ridge (KR) and is connected to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Grímsvötn
Grímsvötn (; ''vötn'' = "waters", singular: ) is a volcano with a (partially subglacial) fissure system located in Vatnajökull National Park, Iceland. The volcano itself is completely subglacial and located under the northwestern side of the Vatnajökull ice cap. The subglacial caldera is at , at an elevation of . Beneath the caldera is the magma chamber of the Grímsvötn volcano. Grímsvötn is a basaltic volcano which has the highest eruption frequency of all the volcanoes in Iceland and has a southwest-northeast-trending fissure system. The massive climate-impacting Laki fissure eruption of 1783–1784 was a part of the same fissure system. Grímsvötn was erupting at the same time as Laki during 1783, but continued to erupt until 1785. Because most of the volcanic system lies underneath Vatnajökull, most of its eruptions have been subglacial and the interaction of magma and meltwater from the ice causes phreatomagmatic explosive activity. Jökulhlaup Eruptions in the c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Theistareykjarbunga
Theistareykjarbunga (Þeistareykjarbunga, ) is a shield volcano in northeastern Iceland with two fissure vents called Þeistareykjahraun and Borgahraun , and two cones: the 370-metre Stórahversmór and the 540-metre-high, 30-km3 Stóravíti . They both are currently extinct. Eruptions There have been three dated eruptions, all VEI-0: the most recent eruption was around 900 BCE and the previous eruption was in 6800 BCE. Around 9500 BCE, an eruption produced approximately 18 billion cubic metres of basaltic lava. See also * List of volcanoes in Iceland This list of volcanoes in Iceland includes active and dormant volcanic mountains, of which 18 have erupted since human settlement of Iceland began around 900 AD. __TOC__ List Volcanic zones and systems Iceland has four major volcanic ... References Shield volcanoes of Iceland North Volcanic Zone of Iceland Polygenetic shield volcanoes Volcanic systems of Iceland Calderas of Iceland Central volcanoes of Ic ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pleistocene
The Pleistocene ( , often referred to as the '' Ice age'') is the geological epoch that lasted from about 2,580,000 to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was finally confirmed in 2009 by the International Union of Geological Sciences, the cutoff of the Pleistocene and the preceding Pliocene was regarded as being 1.806 million years Before Present (BP). Publications from earlier years may use either definition of the period. The end of the Pleistocene corresponds with the end of the last glacial period and also with the end of the Paleolithic age used in archaeology. The name is a combination of Ancient Greek grc, label=none, πλεῖστος, pleīstos, most and grc, label=none, καινός, kainós (latinized as ), 'new'. At the end of the preceding Pliocene, the previously isolated North and South American continents were joined by the Isthmus of Panama, causing a faunal interchange between the t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Grensdalur
Grensdalur () is a volcano in Iceland. The elevation is about 497 m (1631 ft). Its position is 64.02°N 21.17°W. It was active during Pleistocene The Pleistocene ( , often referred to as the '' Ice age'') is the geological epoch that lasted from about 2,580,000 to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was finally confirmed .... References External links * Volcanoes of Iceland Pleistocene stratovolcanoes {{Iceland-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fremrinámur
Fremrinámur () is a volcano with a volcanic system located on the basalt plateau in Iceland. It is at the junction of the Mid-Atlantic Ridge The Mid-Atlantic Ridge is a mid-ocean ridge (a divergent or constructive plate boundary) located along the floor of the Atlantic Ocean, and part of the longest mountain range in the world. In the North Atlantic, the ridge separates the North A ... and the Greenland–Iceland–Faeroe Ridge. It is one of five volcanic systems found in the axial rift zone in north east Iceland. The elevation is about 939 m (3081 ft). The last eruption was in 800 BC (± 300 years). References External links * {{DEFAULTSORT:Fremrinamur Volcanoes of Iceland Volcanic systems of Iceland North Volcanic Zone of Iceland ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Esjufjöll
The subglacial Esjufjöll () volcano is located at the SE part of the Vatnajökull icecap. Esjufjöll is a strict nature reserve (IUCN category Ia). Geography The mountains, actually nunataks within Vatnajökull, are located to the north of Öræfajökull volcano and of Jökulsárlón glacial lake. The mountain range consists of 4 mountain massifs with three valleys in between them.Ari Trausti Guðmundsson, Pétur Þorsteinsson: Íslensk fjöll. Gönguleiðir á 151 tind. Reykjavík 2004, p. 200. The glaciers flowing around them are feeding Breiðamerkurjökull and in the end Jökulsárlón. Volcanism Esjufjöll are a small volcanic system and as such part of Iceland's Oræfi Volcanic Belt. Also part of this zone are Öræfajökull and Snæfell (north of Vatnajökull).See eg.: Thor Thordarson, Armann Hoskuldsson: Classic geology in Europe 3. Iceland. Harpenden 2002, p. 14 The volcanic system consists of the Snaehetta central volcano with a large caldera. Most of the volcan ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Katla (volcano)
Katla () is a large volcano in southern Iceland. It is very active; twenty eruptions have been documented between 930 and 1918, at intervals of 20–90 years. It has not erupted violently for years, although there may have been small eruptions that did not break the ice cover, including ones in 1955, 1999, and 2011. Prior eruptions have had a Volcanic Explosivity Index (VEI) of between 4 and 6 on a scale of 0 to 8. In comparison, the Eyjafjallajökull 2010 eruption had a VEI of 4. Bigger VEI-5 eruptions are comparable to Mount St. Helens 1980 eruption, while significantly rarer VEI-6 eruptions would be comparable to Krakatoa's 1883 eruption and Mount Pinatubo's 1991 eruption. Katla is one of the largest volcanic sources of carbon dioxide (CO2) on Earth, accounting for up to 4% of total global volcanic carbon dioxide emissions. Geography and physical appearances Katla is one of the largest volcanoes in Iceland. It is situated to the north of Vík í Mýrdal and to the ea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eldgjá
Eldgjá (, "fire canyon") is a volcano and a canyon in Iceland. Eldgjá is part of the Katla volcano; it is a segment of a long chain of volcanic craters and fissure vents that extends northeast away from Katla volcano almost to the Vatnajökull ice cap. This fissure experienced a major eruption around 939 CE, which was the largest effusive eruption in recent history. It covered about of land with of lava from two major lava flows. While Icelandic records about the effects of the eruption are sparse, paleoclimate proxies and historical records from China, Europe and the Islamic world describe widespread impacts on the Northern Hemisphere climate. The Eldgjá eruption produced a noticeable cooling of the climate, with resulting cold winters and food crises across Eurasia. Geology The interaction between the Mid-Atlantic Ridge and the Iceland hotspot has given rise to the stack of volcanic rocks that forms Iceland. Volcanoes on Iceland occur in four volcanic zones; the North ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Heimaey
Heimaey (), is an Icelandic island. At , it is the largest island in the Vestmannaeyjar archipelago, and the largest and most populated island off the Icelandic coast. Heimaey is off the south coast of Iceland. It is the only populated island of the Vestmannaeyjar islands, with a population of 4,414. The Vestmannaeyjar Airport and the Westman Islands Golf Club taken together cover a good portion of the island. In January 1973, lava flow from nearby Eldfell destroyed half the town and threatened to close its harbour, its main income source. An operation to cool the advancing lava with sea water saved the harbour. History Abducted from the north of Ireland, the slaves were called westmen (Vestmenn), as before discovering Iceland, Ireland was the most western part of the world known to northern Europeans then (c. 840). The slaves went ashore at Heimaey and took shelter in the hills. Ingólfur hunted them and killed them in revenge for their murdering his foster brother. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Brennisteinsfjöll
Brennisteinsfjöll (, "Sulfur mountains" Brennisteinsfjöll. Detailed description. In: Catalogue of Icelandic Volcanoes. Retrieved 27 July 2020) is a minor Volcanism of Iceland, volcanic system, with s and small es on the Reykjanes Peninsula in southwest |
Geographic Coordinate System
The geographic coordinate system (GCS) is a spherical or ellipsoidal coordinate system for measuring and communicating positions directly on the Earth as latitude and longitude. It is the simplest, oldest and most widely used of the various spatial reference systems that are in use, and forms the basis for most others. Although latitude and longitude form a coordinate tuple like a cartesian coordinate system, the geographic coordinate system is not cartesian because the measurements are angles and are not on a planar surface. A full GCS specification, such as those listed in the EPSG and ISO 19111 standards, also includes a choice of geodetic datum (including an Earth ellipsoid), as different datums will yield different latitude and longitude values for the same location. History The invention of a geographic coordinate system is generally credited to Eratosthenes of Cyrene, who composed his now-lost '' Geography'' at the Library of Alexandria in the 3rd centur ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
.jpeg/1200px-Eldgjá_Volcanic_Canyon_Iceland_(176657459).jpeg "Click for more on -> Eldgjá")
