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Bárðarbunga (Icelandic pronunciation: [ˈpaurðarˌpuŋka] (listen)),[1] is a stratovolcano located under Vatnajökull in Vatnajökull National Park which is Iceland's most extensive glacier. The second highest mountain in Iceland, 2,009 metres (6,591 ft) above sea level, Bárðarbunga is also part of a volcanic system that is approximately 200 kilometres (120 mi) long and 25 kilometres (16 mi) wide.

Bárðarbunga
Eruption at Holuhraun, September 4, 2014
Highest point
Elevation	2,009 m (6,591 ft)
Prominence	550 m (1,800 ft)
Coordinates	64°38′28″N 17°31′41″W
Geography
Bárðarbunga Map of Iceland showing the location of Bárðarbunga.
Location	Vatnajökull, Iceland
Geology
Age of rock	over 10000 years
Mountain type	Subglacial volcano/Icelandic stratovolcano
Last eruption	29 August 2014 to 27 February 2015

Description

Bárðarbunga is a subglacial stratovolcano[2] under the ice cap of Vatnajökull glacier in the Vatnajökull National Park in Iceland. It rises to 2,009 metres (6,591 ft) above sea level, making it the second highest mountain in Iceland, about 101 metres (331 ft) lower than Hvannadalshnjúkur. The caldera is about 80 square kilometres, up to 10 km wide and about 700 metres (2,300 ft) deep.[2] 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.[3]

Bárðarbunga was a little-known volcano in Iceland due to its remote location and infrequent eruptions approximately once every 50 years, but recent studies have shown that many tephra layers originally thought to be from other volcanoes were ejected from Bárðarbunga.

Sustained seismic activity has been gradually increasing in Bárðarbunga and its associated northern fissure system for seven years starting in 2007 and leading to an eruption towards the end of 2014. This activity decreased after the Grímsvötn eruption in 2011, but later returned to a similar level as before the eruption. The previous eruption was in 1910. There has been frequent volcanic activity outside the glacier to the southwest in the highlands between Vatnajökull and Mýrdalsjökull, and also to the northeast toward Dyngjufjöll [ˈtɪɲcʏˌfjœtl̥].

Etymology

Bárðarbunga is named after an early Icelandic settler named Gnúpa-Bárður [ˈknuːpa-ˌpaurðʏr̥], and literally translates as "Bárður's bulge" or "Bárður's bump" since "Bárðar" is the genitive case of "Bárður".[4]

Eruptions and notable activity

Throughout history there have been large eruptions every 250–600 years. In 1477, the largest known eruption from Bárðarbunga had a volcanic explosivity index (VEI) of 6; there is evidence of many smaller eruptions during the past 10,000 years.[2]

6600 BC

Þjórsá Lava, the largest Holocene lava flow on earth,[2] originated from Bárðarbunga about 8,600 years ago, with a total volume of 21[2] to 30 cubic kilometres and covering approximately 950 square kilometres.[5]

870

Many large eruptions have occurred south-west of the glacier; the first occurring since human settlement of Iceland was the Vatnaöldur eruption about 870 which had a volcanic explosivity index (VEI) of 4.[2]

1477

The Veiðivötn eruption in 1477 is the largest known Icelandic eruption, with a VEI of 6.[2]

1701–1864

Studies of tephra layers have shown that a number of eruptions have occurred beneath the glacier, probably in the north-east of the crater or in Bárðarbunga. There have also been smaller eruptions in an ice-free area of Dyngjuháls [ˈtiɲcʏˌhauls] to the north-east. Eruptions appear to follow a cycle: there were several eruptions in the glacier between 1701 and 1740 and since 1780.

1910 eruption

1910 was the last known eruption of Bárðarbunga before the 2014 eruptions.[6]

1996

The Gjálp fissure vent eruption in 1996 revealed that an interaction may exist between Bárðarbunga and Grímsvötn. A strong earthquake in Bárðarbunga, about 5 on the Richter scale, is believed to have started the eruption in Gjálp. On the other hand, because the magma erupted showed strong connections to the Grímsvötn Volcanic System as petrology studies showed, the 1996 as well as a former eruption in the 1930s are thought to have taken place within Grímsvötn Volcanic system.[7]

2010

On 26 September 2010, an earthquake swarm was recorded with over 30 earthquakes measuring up to 3.7M_W on the moment magnitude scale.^{[citation needed]}

2014–2015

In August 2014, a swarm of around 1,600 earthquakes in 48-hours, with magnitudes up to 4.5M_W, [8][9] was followed on 23 August by the USGS Aviation Color Codes being raised from orange to red, indicating an eruption in progress.[10] The following day, the aviation risk was lowered from red to orange and the statement that there was an eruption in progress was retracted.[11] However, later aerial observations of glacial depressions southeast of the volcano suggested that the now-retracted report of an eruption had been correct and that a short eruption did occur under the ice, but the lack of further melting indicated that this eruption had now ceased. Then, a new fissure eruption breached the surface between Bárðarbunga and Askja, in the Holuhraun lava field, in the early hours of 29 August.[12] This was followed by a second fissure eruption in the Holuhraun area, along the same volcanic fissure, which started shortly after 4 am on 31 August.[13]

The eruption emitted large volumes of sulphur dioxide and impacted air quality in Iceland. There was no effect on flights outside of the immediate vicinity as the eruption hadn't produced a significant amount of volcanic ash.

On February 28, 2015 it was officially reported that the eruption was over.[14] Nevertheless, the gas pollution still existed, and the area north of Bárðarbunga, including volcanoes Askja and Herðubreið, still remained closed for visitors.

On March 16, 2015 the area north of Bárðarbunga was opened for visitors, excluding the new lava field and the area within 20 metres around it.[15]

1950 Geysir air crash

On 14 September 1950 a Douglas C-54 Skymaster aircraft belonging to the Icelandic airline Loftleiðir crash landed on the Vatnajökull glacier at Bárðarbunga during a cargo flight from Luxembourg to Reykjavík.[16] There were no fatalities, but damaged radio equipment left them unable to communicate their location. After two days the crew managed to reach the emergency transmitter in the plane's rubber liferaft and send out an distress call which was picked up by the Icelandic Coast Guard vessel Ægir. The same day a search and rescue Catalina aircraft, named Vestfirðingur, spotted them. The C-54's cargo included the body of a deceased United States Air Force (USAF) colonel, prompting American assistance. A USAF C-47 equipped with skis landed on the glacier but was unable to take off again, so it had to be abandoned. After six days both crews were rescued by a ski-patrol from Akureyri. Later Loftleiðir bought the stranded C-47 from the USAF for $700.[17] In April 1951 it was dug out of the snow and towed down the mountain by two bulldozers, where it was started and flown to Reykjavík.[18][19][20]

See also

• List of volcanoes in Iceland
• Timeline of volcanism on Earth
• Volcanism of Iceland

References

External links

• Bárðarbunga in the Catalogue of Icelandic Volcanoes
• 3d map of volcanic activity and webcam at Bárðarbunga updated live from IMO
• Bárðarbunga live webcams feed
• Michigan Tech Geological Engineering and Sciences – Bárðarbunga/Grimsvötn Volcanoes
• Seismic activity in the Vatnajökull region
• Bárðarbunga volcano livestream
• (The Bárðarbunga System), pre-publication extract from The Catalogue of Icelandic Volcanoes
• Official Website of Vatnajökull National Park

На других языках

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[de] Bárðarbunga

Die Bárðarbunga (Bardarbunga,  [.mw-parser-output .IPA a{text-decoration:none}ˈb̥aurðarˌb̥uŋg̥a]) ist ein subglazialer Zentralvulkan mit Caldera unter dem Gletscher Vatnajökull in Island. Sie erreicht eine Höhe von 2010 m, womit sie der zweithöchste Berg Islands ist. Mit den angeschlossenen Spaltensystemen bildet sie auch das gleichnamige Vulkansystem. Die bisher letzte Eruption des Vulkans dauerte von August 2014 bis Februar 2015.

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- [en] Bárðarbunga

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[es] Bárðarbunga

Bárðarbunga ( ['b̥aurðarˌb̥uŋg̥a] (?·i)) es un estratovolcán[1] activo situado bajo la capa de hielo del glaciar Vatnajökull, el más extenso de Islandia. Se levanta a unos 2 mil msnm, lo que lo convierte en la segunda montaña más alta de Islandia, sólo unos 10 m por debajo del Hvannadalshnjúkur. Forma parte de un sistema volcánico de 200 km de longitud y 25 km de ancho. La última vez que entró en erupción fue en 1910. Sin embargo, en agosto de 2014, el volcán comenzó a dar signos de creciente actividad sísmica lo que forzó a las autoridades aeronáuticas islandesas a emitir diversas alertas. Sus erupciones llegaron a alterar el tiempo meteorológico y el tráfico aéreo en el hemisferio norte de la Tierra.[1]

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[fr] Bárðarbunga

Le Bárðarbunga (prononcé [ˈpaurðarpuŋka] .mw-parser-output .prononciation>a{background:url("//upload.wikimedia.org/wikipedia/commons/thumb/8/8a/Loudspeaker.svg/11px-Loudspeaker.svg.png")center left no-repeat;padding-left:15px;font-size:smaller}écouter), toponyme islandais signifiant littéralement en français « bosse de Bárður » (prénom islandais), aussi appelé Bárðarbunga-Veiðivötn du nom d'une fissure volcanique associée au volcan central, est un volcan d'Islande situé sous le Vatnajökull, la plus grande calotte glaciaire du pays. Second plus haut volcan d'Islande, il est voisin du Grímsvötn, un autre volcan sous-glaciaire connu pour ses jökulhlaups.

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[it] Bárðarbunga

Il Bárðarbunga (ˈbaurðarbuŋka),[1][2], o Bardarbunga (traslitterato in italiano), è uno stratovulcano subglaciale[3] situato sotto la cappa di ghiaccio del Vatnajökull, il più vasto ghiacciaio islandese.Il Bárðarbunga fa parte di un sistema vulcanico lungo circa 200 km e largo 25 km.

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[ru] Баурдарбунга

Ба́урдарбунга, встречается также написание Бардарбунга (исл. Bárðarbunga, ['baurðarbuŋka][2]) — подлёдный вулкан в районе Нордюрланд-Эйстра на юго-востоке Исландии. Включает в себя близлежащие объекты: стратовулканы, вулканические разломы, вулканические хребты, кратеры. До 2014 года последнее извержение наблюдалось в 1910 году, последнее крупное извержение произошло в 1477 году.mw-parser-output .ts-Переход img{margin-left:.285714em}[⇨]. В августе 2014 года началось новое извержение вулкана, которое продолжалось до начала 2015 года[⇨].

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