Gígjökull, Eyjafjallajökull's largest outlet glacier covered in volcanic ash
|Elevation||1,651 m (5,417 ft)|
|Pronunciation||Icelandic pronunciation: [ˈeɪjaˌfjatlaˌjœːkʏtl̥]|
|Volcanic arc/belt||East Volcanic Zone|
|Last eruption||March to June 2010|
Eyjafjallajökull (pronounced [ˈeɪjaˌfjatlaˌjœːkʏtl̥] ( ); Icelandic for "glacier of Eyjafjöll") is one of the smaller ice caps of Iceland, situated to the north of Skógar and to the west of Mýrdalsjökull. The ice cap covers the caldera of a volcano with a summit elevation of 1,651 metres (5,417 ft). The volcano has erupted relatively frequently since the last glacial period, most recently in 2010.
Eyjafjallajökull consists of a volcano completely covered by an ice cap. The ice cap covers an area of about 100 square kilometres (39 sq mi), 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 (or 1:47:55 PM) there was an explosion on the glacier. It can be timed because the seismometers in Kirkjubæjarklaustur monitored the movement. When about 15,000,000 cubic metres (529,720,001 cubic feet) of material hit the glacier a massive amount of air, ice, and water began to move from under the glacier out into the lagoon at the foot of the glacier.
The mountain itself, a stratovolcano, stands 1,651 metres (5,417 ft) at its highest point, and has a crater 3–4 kilometres (1.9–2.5 mi) in diameter, open to the north. The crater rim has three main peaks, being (clockwise from the north-east) Guðnasteinn, 1,500 metres (4,900 ft) (approx), Hámundur, 1,651 metres (5,417 ft) and Goðasteinn, 1,497 metres (4,911 ft). The south face of the mountain was once part of Iceland's Atlantic coastline, from which, over thousands of years, the sea has retreated some 5 kilometres (3.1 mi). The former coastline now consists of sheer cliffs with many waterfalls, of which the best known is Skógafoss. In strong winds, the water of the smaller falls can even be blown up the mountain. The area between the mountain and the present coast is a relatively flat strand, 2 to 5 km (1 to 3 miles) wide, called Eyjafjöll.
The volcano is fed by a magma chamber under the mountain, which in turn derives from the tectonic divergence of the Mid-Atlantic Ridge. It is part of a chain of volcanoes stretching across Iceland. Its nearest active neighbours are Katla, to the northeast, and Eldfell, on Heimaey, to the southwest. The volcano is thought to be related to Katla geologically, in that eruptions of Eyjafjallajökull have generally been followed by eruptions of Katla.
The Eyjafjallajökull volcano erupted in 920, 1612 and again from 1821 to 1823 when it caused a glacial lake outburst flood (or jökulhlaup). It erupted three times in 2010—on 20 March, April–May, and June. The March event forced a brief evacuation of around 500 local people, but the 14 April eruption was ten to twenty times more powerful and caused substantial disruption to air traffic across Europe. It caused the cancellation of thousands of flights across Europe and to Iceland.
The name means "glacier" (or more properly here "ice cap") of the Eyjafjöll. The word jökull, meaning glacier or ice cap, is cognate with the Middle English word ikel surviving in the -icle of English icicle).
Eyjafjöll is the name given to the southern side of the volcanic massif together with the small mountains which form the foot of the volcano.
The name Eyjafjöll is made up of the words eyja (genitive plural of ey, meaning eyot or island), and the plural word fjöll, meaning fells or mountains), and together literally means: "the mountains of the islands". The name probably refers to the close-by archipelago of Vestmannaeyjar.
The word fjalla is the genitive plural of fjöll, and so Eyjafjalla is the genitive form of Eyjafjöll and means: "of the Eyjafjöll". A literal part-by-part translation of Eyjafjallajökull would thus be "Islands' Mountains' ice cap".
The stratovolcano, whose vents follow an east-west trend, is composed of basalt to andesite lavas. Most of its historical eruptions have been explosive. However, fissure vents occur on both (mainly the west) sides of the volcano.
1821 to 1823 eruptions
Some damage was caused by a minor eruption in 1821. Notably, the ash released from the eruption contained a large fraction of fluoride, which in high doses may harm the bone structure of cattle, horses, sheep and humans. The eruption also caused some small and medium glacier runs and flooding in nearby rivers Markarfljót and Holtsá. The eruptive phase started on 19 and 20 December 1821 by a series of explosive eruptions and continued over the next several days. The sources describe heavy ash fall in the area around the volcano, especially to the south and west.
After that event the sequence of eruptions continued on a more subdued level until June 1822.
From the end of June until the beginning of August 1822, another sequence of explosive eruptions followed. The eruption columns were shot to considerable heights, with ashfall in both the far north of the country, in Eyjafjörður, and in the southwest, on the peninsula of Seltjarnarnes near Reykjavík.
The period from August to December 1822 seemed quieter, but farmers attributed the death of cattle and sheep in the Eyjafjörður area to poisoning from this eruption, which modern analysis identifies as fluoride poisoning. Some small glacier runs occurred in the river Holtsá. A bigger one flooded the plains near the river Markarfljót. The sources do not indicate the exact date.
In April 2010, seismic activity was detected in the volcano area, with thousands of small earthquakes (mostly magnitude 1–2 on the Richter magnitude scale, with only a couple greater than 3 magnitude) 7–10 kilometres (4.3–6.2 mi) beneath the volcano. On 26 February 2010, unusual seismic activity along with rapid expansion of the Earth's crust was registered by the Meteorological Institute of Iceland. This gave geophysicists evidence that magma was pouring from underneath the crust into the magma chamber of the Eyjafjallajökull volcano and that pressure stemming from the process caused the huge crustal displacement at Þorvaldseyri farm. The seismic activity continued to increase and from 3–5 March, close to 3,000 earthquakes were measured at the epicenter of the volcano.
The eruption is thought to have begun on 20 March 2010, about 8 kilometres (5.0 mi) east of the top crater of the volcano, on Fimmvörðuháls, the high neck between Eyjafjallajökull and the neighbouring icecap, Mýrdalsjökull. This first eruption, in the form of a fissure vent, did not occur under the glacier and was smaller in scale than had been expected by some geologists. The fissure opened on the north side of Fimmvörðuháls, directly across the popular hiking trail between Skógar, south of the pass, and Þórsmörk, immediately to the north.
On 14 April 2010 Eyjafjallajökull resumed erupting after a brief pause, this time from the top crater in the centre of the glacier, causing jökulhlaup (also known as meltwater floods) to rush down the nearby rivers, and requiring 800 people to be evacuated. This eruption was explosive in nature, due to melt water getting into the volcanic vent. It was estimated to be ten to twenty times larger than the previous one in Fimmvörðuháls. This second eruption threw volcanic ash several kilometres up in the atmosphere which led to air travel disruption in northwest Europe for six days from 15 April to 21 April 2010 and also in May 2010,[clarification needed] including the closure of airspace over many parts of Europe. The eruptions also created electrical storms. On 23 May 2010, the London Volcanic Ash Advisory Commission declared the eruption to have stopped, but stated that they were continuing to monitor the volcano. The volcano continued to have several earthquakes daily, with Volcanologists watching the volcano closely. As of August 2010, Eyjafjallajökull was considered dormant.
Relationship to Katla
Eyjafjallajökull lies 25 km (16 mi) west of another subglacial volcano, Katla, under the Mýrdalsjökull ice cap, which is much more active and known for its powerful subglacial eruptions and its large magma chamber. Each of the eruptions of Eyjafjallajökull in 920, 1612, and 1821–1823 has preceded an eruption of Katla. Katla has not displayed any unusual activity (such as expansion of the crust or seismic activity) during the 2010 eruptions of Eyjafjallajökull, though geologists have been concerned about the general instability of Katla since 1999. Some geophysicists in Iceland believe that the Eyjafjallajökull eruption may trigger an eruption of Katla, which would cause major flooding due to melting of glacial ice and send up massive plumes of ash. On 20 April 2010, Icelandic President Ólafur Grímsson said "the time for Katla to erupt is coming close...we [Iceland] have prepared...it is high time for European governments and airline authorities all over the world to start planning for the eventual Katla eruption".
Volcanologists continue to monitor Katla, aware that any eruption from Katla following an eruption from Eyjafjallajökull has historically occurred within months of an Eyjafjallajökull eruption. The Icelandic Meteorological Office updates its website with reports of quakes both at Eyjafjallajökull and Katla. A small eruption of Katla was confirmed on 8 July 2011, after a harmonic tremor was detected. The event produced cracks on Katla's glacier and a jökulhlaup that destroyed a bridge on the Ring Road.
- Glaciers of Iceland
- Volcanism of Iceland
- Waterfalls of Iceland
- Ragnar Th. Sigurdsson who photographed the 2010 eruption
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|Wikimedia Commons has media related to Eyjafjallajökull.|
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- Photos & Videos from Eyjafjallajökull
- Satellite image of 2010 eruption by NASA
- Photos of the 2010 eruption by Fred Kamphues
- A collection of satellite images from the CIMSS Satellite Blog
- Best of Photo Collection
- More from Eyjafjallajökull – The Big Picture
- Photographs by Raw Iceland, a Reykjavík-based organization that organizes amateur and professional photography tours to the volcano
- Videos and webcams
- Webcams of the eruption
- A short time-lapse from April 17, 2010. About 30 minutes played in 18 second.
- Video of the first 2010 eruption
- Video of the first 2010 eruption by Raw Iceland
- Video of the aftermath of Eyjafjallajokull eruption. Shot on July 28, 2010
- A film crew lands on Eyjafjallajokull during the 2010 eruption
- Volcanic Eyjafjallajökull run off: Seljalandsfoss Waterfall (binaural recording optimized for headphones)
- Geological articles
- Univ. of Iceland: History of Eyjafjallajökull (Icelandic)
- Geology of Katla and Eyjafjallajökull volcanoes, University of Iceland
- Magma pathways and earthquakes at Eyjafjallajökull, Icelandic Meteorological Institute (PDF)
- Institute of Earth Sciences – Eruption in Eyjafjallajökull (daily eruption status reports)
- SI / USGS Weekly Volcanic Activity Report for Eyjafjallajökull
- Aviation ash forecasts
- Volcanic Ash Advisory Graphical Forecast for the North Atlantic region
- Volcanic Ash Concentration Charts for the North Atlantic region