2010 eruptions of Eyjafjallajökull

Dust particles that get suspended in the atmosphere scatter light from the setting sun, generating 'volcanic lavenders' like this one over the flight path of Leeds-Bradford Airport in England during the aviation shutdown

Eyjafjallajökull (pronounced [ˈɛɪjaˌfjatl̥aˌjœːkʏtl] (listen)) is one of Iceland's smaller ice caps located in the far south of the island. Situated to the north of Skógar and to the west of the larger ice cap Mýrdalsjökull, Eyjafjallajökull covers the caldera of a volcano 1,666 m (5,466 ft) high, which has erupted relatively frequently since the last ice age. The most recent major eruptions occurred in 920, 1612, and from 1821 to 1823.[8] Previous eruptions of Eyjafjallajökull have been followed by eruptions at its larger neighbour, Katla.[9] 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."[10]

The volcanic events starting in March 2010 were considered to be a single eruption divided into phases. The first eruption phase ejected olivine basaltic andesite lava[11] several hundred metres into the air in what is known as an effusive eruption. Ash ejection from this phase of the eruption was small, rising to no more than 4 km (2.5 mi) into the atmosphere.

On 14 April 2010, however, the eruption entered an explosive phase and ejected fine glass-rich ash to over 8 km (5.0 mi) into the atmosphere. The second phase was estimated to be a VEI 4 eruption, which was large, but not nearly the most powerful eruption possible by volcanic standards. By way of comparison, the Mount St. Helens eruption of 1980 was rated as 5 on the VEI, and the 1991 eruption of Mount Pinatubo was rated as a 6. This second phase erupted trachyandesite.[12]

This volcanic activity so disruptive to air travel because of a combination of factors:

1. The volcano was directly under the jet stream.
2. The direction of the jet stream was unusually stable at the time of the eruption's second phase, continuously southeast.
3. The second eruptive phase happened under 200 m (660 ft) of glacial ice. The resulting meltwater flowed back into the erupting volcano, which created two specific phenomena:
   1. The rapidly vaporising water significantly increased the eruption's explosive power.
   2. The erupting lava cooled very fast, which created a cloud of highly abrasive, glass-rich ash.
4. The volcano's explosive power was enough to inject ash directly into the jet stream.

People observing the first fissure at Fimmvörðuháls

"Volcano tourism" quickly sprang up in the wake of the eruption, with local tour companies offering day trips to see the volcano.[13] The Civil Protection Department[14] of the Icelandic Police produced regular reports about access to the area, including a map of the restricted area around Eyjafjallajokull, from which the public was forbidden. Teams from the Icelandic Association for Search and Rescue were stationed at the eruption site as part of standard safety measures and to assist in enforcing access restrictions.

Vodafone and the Icelandic telecommunications company Míla installed webcams, giving views of the eruption from Valahnúkur, Hvolsvöllur, and Þórólfsfell. The view of the eruption from Þórólfsfel also includes a thermal imaging camera.

The London Volcanic Ash Advisory Centre (VAAC),[15] part of the UK Met Office, was responsible for forecasting the presence of volcanic ash in the north-east Atlantic. All ash dispersion models for this geographic region were produced by the VAAC in London.

A study by the Icelandic Meteorological Office published on December 2009 indicated an increase in seismic activity around the Eyjafjallajökull area during the years 2006–2009. The study reported increased activity that occurred between June and August 2009 (200 events), compared to a total of about 250 earthquakes recorded between September 2006 and August 2009. It further indicated that the locations of most of the earthquakes in 2009 occurred between 8 to 12 km (5.0 to 7.5 mi) depth east of the volcano's top crater.[16] At the end of December 2009, seismic activity began around the Eyjafjallajökull volcano area, with thousands of small earthquakes (mostly of magnitude 1–2 M_w), 7 to 10 km (4.3 to 6.2 mi) beneath the volcano.[17]

The radar stations of the Meteorological Institute of Iceland did not detect any appreciable amount of volcanic ashfall during the first 24 hours of the eruption.[18] However, during the night of 22 March, they reported some volcanic ash fall reaching the Fljótshlíð area (20 to 25 km (12 to 16 mi) north-west of the eruption's location)[19] and Hvolsvöllur town (40 kilometres (25 mi) north-west of the eruption location)[19] leaving vehicles with a fine, grey layer of volcanic ash. At around 07:00 on 22 March, an explosion launched eruption columns as far as 4 km (2.5 mi) straight up into the air. This was the highest plume since the eruption started.[20] On 23 March, a small vapour explosion took place, when hot magma came into contact with nearby snowdrifts, emitting a vapour plume which reached an altitude of 7 km (4.3 mi), and was detected on radar from the Meteorological Institute of Iceland. After that, many further vapour explosions occurred.[21]

By 26 February 2010, the global positioning system (GPS) equipment used by the Iceland Meteorological Office[22] at Þorvaldseyri farm in the Eyjafjöll area (around 15 km (9.3 mi) south-east of the location of the recent eruption)[19] had shown 3 cm of displacement of the local crust in a southward direction, of which a 1-cm displacement had taken place within four days. (See the GPS Time Series[23] page of the Nordic Volcanological Center's[24] website for detailed information on the degree of movement detected in the Earth's crust in the Eyjafjallajökull locality.)

This unusual seismic activity, along with the rapid movement of the Earth's crust in the area, gave geophysicists evidence that magma was flowing from underneath the crust into Eyjafjallajökull's magma chamber and that pressure stemming from the process caused (in geophysical terms) the huge crustal displacement at Þorvaldseyri farm.[25] The seismic activity continued to increase, and from 3 to 5 March, close to 3,000 earthquakes were measured having their epicentre at the volcano. Most of these were too small (magnitude 2) to be interpreted as precursors to an eruption, but some could be detected in nearby towns.[26]

The grounding of European flights avoided about 3.44×10⁸ kg of CO₂ emissions per day, while the volcano emitted about 1.5×10⁸ kg of CO₂ per day.[27]

The first phase of the eruption lasted from 20 March to 12 April 2010 and was characterised by olivine basaltic andesite lava flowing from various eruptive vents on the flanks of the mountain.

Fissure

Second fissure, viewed from the north, on 2 April 2010

The first phase of the 2010 eruption began late on the evening of 20 March at the Eyjafjallajökull.

The initial visual report of the eruption was at 23:52 GMT, when a red cloud was seen at the north slopes of Fimmvörðuháls mountain pass,[38][39] lighting up the sky above the eruptive site. The eruption was preceded by intense seismicity and high rates of deformation in the weeks before the eruption, in association with magma recharging of the volcano. Immediately before the eruption, the depth of the seismicity had become shallow, but was not significantly enhanced from what it had been in the previous weeks. Deformation was occurring at rates up to a centimetre a day since 4 March at various GPS sites installed within 12 km (7.5 mi) from the eruptive site.

A fissure opened up about 150 metres (490 ft) in length running in a north-east to south-west direction, with 10 to 12 erupting lava craters ejecting lava at a temperature around 1,000 °C (1,800 °F) up to 150 m (490 ft) into the air. The lava was alkali olivine basalt[40] and was relatively viscous, causing the motion of the lava stream to the west and east of the fissure to be slow. The molten lava flowed more than 4,000 m (13,000 ft) to the north-east of the fissure and into Hrunagil canyon, forming a lava fall more than 200 m (660 ft) long and slowly approaching Þórsmörk, but had not yet reached the flood plains of Krossá.[41][42][43]

On 25 March 2010, while studying the eruption, scientists witnessed, for the first time in history, the formation of a pseudocrater during a steam explosion.[44] Crustal expansion continued at Þorvaldseyri for two days after the eruption began, but was slowly decreasing whilst the volcanic activity was increasing. This indicates that the rate at which magma was flowing into the magma chamber roughly equaled the rate at which it was being lost due to the eruption, giving evidence that this phase of volcanic activity reached equilibrium.[45]

A new fissure opened on 31 March, around 200 m (660 ft) north-west of the original fissure.[46] Many witnesses were present while the new fissure opened. It was a bit smaller, around 300 m (980 ft) long according to witnesses, and lava coming from it started to flow into Hvannárgil canyon. These two erupting fissures shared the same magma chamber, according to geophysicists. No unusual seismic activity was detected at the time the new fissure appeared, nor any crustal expansion according to many seismometers and GPS recorders situated in nearby areas.[47][48]

Geophysicist Magnús Tumi Einarsson said (at a press meeting in Hvolsvöllur on 21 March) that this eruption was small compared to, for example, the eruption of Hekla in 2000. The eruption, rather than taking place under the ice cap of the glacier, occurred in the mountain pass between the Eyjafjallajökull and Mýrdalsjökull glaciers. As long as the fissure was not near the glacier, the risk of flooding was minimal; however, the fissure could extend into the ice cap, thereby greatly increasing the risk of flooding.[49]

Photograph from satellite Aqua showing the ash plume over North Atlantic at 13:30 GMT on 15 April

The estimated ash cloud at 18:00 GMT on 15 April.

After a short hiatus in eruptive activity, and a large increase in seismic activity 23:00 on 13 April and 1:00 on 14 April, a new set of craters opened early in the morning of 14 April 2010 under the volcano's ice-covered central summit caldera. The earthquake swarm was followed by the onset of a seismic eruption tremor. Meltwater started to emanate from the ice cap around 07:00 on 14 April and an eruption plume was observed in the early morning. Visual observations were greatly restricted due to cloud cover over the volcano, but an aeroplane of the Icelandic Coast Guard imaged eruptive craters with radar instruments. A series of vents along a 2-km-long north–south-oriented fissure was active, with meltwater flowing mostly down the northern slopes of the volcano, but also to the south. An ash-loaded eruption plume rose to more than 8 km (5.0 mi), deflected to the east by westerly winds.

Ash analysis

Upper: Ash covers the Thórsmörk valley in early June 2010, immediately after the eruption Lower: The same area, in September 2011

Samples of volcanic ash collected near the eruption showed a silica concentration of 58%—much higher than in the lava flows.[50] The concentration of water-soluble fluoride was one-third of the concentration typical in Hekla eruptions, with a mean value of 104 mg of fluoride per kg of ash. Agriculture is important in this region of Iceland,[51] and farmers near the volcano have been warned not to let their livestock drink from contaminated streams and water sources,[52] as high concentrations of fluoride can have deadly renal and hepatic effects, particularly in sheep.[53]

A necklace made from the ash of the 2010 eruption: Jewellery and similar memorabilia of the eruption are now sold in Iceland.

By the morning of 24 May 2010, the view from the web camera installed on Þórólfsfell[57] showed only a plume of water vapour surrounded by a bluish haze caused by emission of sulphurous gases. Due to the large quantities of dry volcanic ash lying on the ground, surface winds frequently lifted up an "ash mist" that significantly reduced visibility and made web camera observation of the volcano impossible.[58]

On 21 June 2010, data from seismic recorders in the area indicated that the frequency and strength of earth tremors had diminished, but were continuing.[59]

In October 2010, Ármann Höskuldsson, a scientist at the University of Iceland Institute of Earth Sciences, stated that the eruption was officially over, although the area was still geothermally active and might erupt again.[7]

During the eruption, the BBC television news announcers did not try to pronounce the name "Eyjafjallajökull," but called it "the Iceland volcano."

The Institute of Earth Sciences[60] made a preliminary estimate of erupted material in the first three days of the eruption on 14 April 2010 at Eyjafjallajökull. The erupted products were fragmented material, the majority fine-grained airborne tephra. Eruptive products can be split into three categories along with preliminary estimated erupted volumes:

1. Material (tephra) in the ice cauldrons around the volcanic vents: 30 million cubic metres (39,000,000 cu yd)
2. Tephra filling the glacial lagoon of Gígjökulslón, carried by floods down the outlet glacier Gígjökull: 10 million cubic metres (13,000,000 cu yd)
3. Airborne tephra that was carried to the east and south of the volcano, uncompacted tephra fallout from eruption plume: 100 million cubic metres (130,000,000 cu yd)

Total: 140 million cubic metres (180,000,000 cu yd) which corresponds to some 70–80 million cubic metres (92,000,000–105,000,000 cu yd) of magma. The magma discharge rate was about 300 cubic metres per second (11,000 cu ft/s) or 750 t/s. This was 10–20 times the average discharge rate in the preceding flank eruption at Fimmvörðuháls. (First eruption on 20 March 2010).[61]

The IES updated the eruption flow rate on 21 April 2010 to an estimation less than 30 cubic metres per second (1,100 cu ft/s) of magma, or 75 tonnes/s, with a large uncertainty. IES also noted that the eruption continue with less explosive activity.[62]

No human fatalities were reported from the 2010 eruption of Eyjafjallajökull. The people who lived near the volcano had high levels of irritation symptoms, though their lung function was not lower than expected.[63] Six months later, the population living in the area had more respiratory symptoms than a control group from North Iceland, with no ashfall.[64] In Scotland, the number of phone calls to health services for respiratory and eye irritation did not rise significantly.[65]

Volcanic ash is a major hazard to aircraft.[66] Smoke and ash from eruptions reduce visibility for visual navigation, and microscopic debris in the ash can sandblast windscreens and melt in the heat of aircraft turbine engines, damaging engines and making them shut down.[56][66] Many flights within, to, and from Europe were cancelled following 14 April 2010 eruption, and although no commercial aircraft were damaged, the engines of some military aircraft were harmed.[67][68] The presence and location of the plume depends upon the state of the eruption and the winds. While some ash fell on uninhabited areas in Iceland, most had been carried by westerly winds resulting in the shutdown of large air space over Europe. The shutdown had a knock on impact on the economy and cultural events across Europe. The Icelandic flag carrier airline, Icelandair, seemed at first especially vulnerable, but managed to deal effectively with the eruption and subsequently published a detailed report about its actions and conclusions.[69]

Possible ash fallout from Eyjafjallajökull on a car, Manchester, England, 21 April 2010

At the mouth of the crater, the gases, ejecta, and volcanic plume have created a rare weather phenomenon known as volcanic lightning (or a "dirty thunderstorm").[70] When rocks and other ejecta collide with one another, they create static electricity. This, with the abundant water-ice at the summit, aids in making lightning.[71]

High-fluoride Hekla eruptions pose a threat to foraging livestock, especially sheep. Fluoride poisoning can start in sheep at a diet with fluorine content of 25 ppm. At 250 ppm, death can occur within a few days.[53] In 1783, 79% of the Icelandic sheep stock were killed, probably as a result of fluorosis caused by the eruption of Laki.[72] The effect also spread beyond Iceland.[73] Ash from the current Eyjafjallajökull eruption contains one-third the concentration typical in Hekla eruptions, with a mean value of 104 mg of fluoride per kg of ash. Large-scale release of sulphur dioxide into the troposphere also poses a potential health risk, especially to people with pre-existing breathing disorders.

As of 15 April, the eruption was not large enough to have an effect on global temperatures like that of Mount Pinatubo and other major past volcanic eruptions.[74][75] One previous related sequence of eruptions of this volcano, beginning in 1821 is recorded as having lasted for over two years, but no single set of major eruptions is known to have lasted more than 'several days'.

The recent eruptions of Eyjafjallajökull and the largest ash plume associated with the second eruption phase were not unparalleled in either volume or abundance; however, the location was the critical factor because it affected air travel across Europe. Neither phase of the eruption was unusually powerful.[76][77] Other notable volcanic eruptions in recent years include the eruption of Mount Pinatubo of 1991 of VEI 6.[3] This eruption lasted eight days, from 7 – 15 June of that year, with an ash cloud that would have required additional days to dissipate,[78] and resulted in worldwide abnormal weather and decrease in global temperature over the next few years. However, the second phase of Eyjafjallajökull's eruption lasted longer than that of Mount Pinatubo.

• 2010 eruptions of Mount Merapi
• 2014–2015 eruption of Bárðarbunga
• Air travel disruption after the 2010 Eyjafjallajökull eruption
• British Airways Flight 9
• Effects of the April 2010 Eyjafjallajökull eruption
• KLM Flight 867
• Laki
• List of volcanoes in Iceland
• North Atlantic oscillation
• Timeline of volcanism on Earth
• Tuya

Wikimedia Commons has media related to 2010 eruption series in the Eyjafjallajökull volcanic system.

• Frequently Asked Questions on the Eruption in Iceland – from the Icelandic Met Office
• BBC webpage with film of the volcano, taken from 500m from the crater's edge, by Chris Weber on 13 May 2010
• Volcanic Ash and Aviation Safety – SKYbrary guidance to pilots and controllers concerning the effects of volcanic ash.
• Collection of Scientific Earth Observations and Models
• NASA Observes the Icelandic Volcano
• NASA Earth Observatory satellite imagery
• Satellite evidence of hot lava flows from an Icelandic volcano (CIMSS Satellite Blog) (March 2010)
• Description of beginning of current eruption, (March 2010), Icelandic Met Office
• Volcanoes in European history – Podcast placing the Eyjafjallajökull eruption in a historical perspective.
• Webpages and -links related to 2010 Eyjafjallajökull eruptions, Icelandic Met Office