After that, many further vapour explosions occurred. High-fluoride Hekla eruptions pose a threat to foraging livestock, especially sheep. Consequently, a very high proportion of flights within, to, and from Europe were cancelled, creating the highest level of air travel disruption since the Second World War. The earthquake swarm was followed by the onset of a seismic eruption tremor. A short time-lapse from 17 April 2010. These two erupting fissures shared the same magma chamber, according to geophysicists. Photos of the 2010 eruptions by Fred Kamphues, Volcanic Eyjafjallajökull run off: Seljalandsfoss Waterfall (binaural recording optimised for headphones), https://en.wikipedia.org/w/index.php?title=2010_eruptions_of_Eyjafjallajökull&oldid=990444873, Articles with unsourced statements from September 2010, Articles with unsourced statements from August 2010, Articles containing potentially dated statements from April 2010, All articles containing potentially dated statements, Articles with unsourced statements from February 2017, Creative Commons Attribution-ShareAlike License, large-scale disruption to air travel, smaller effects on farming in Iceland. Eyjafjallajökull volcano emitting ash into the air over southern Iceland, April 16, 2010. Articles from Britannica Encyclopedias for elementary and high school students. Beginning on 14 April 2010, the eruption entered a second phase and created an ash cloud that led to the closure of most of the European IFR airspace from 15 until 20 April 2010. [7], Eyjafjallajökull (pronounced [ˈɛɪjaˌfjatl̥aˌjœːkʏtl] (listen)) is one of Iceland's smaller ice caps located in the far south of the island. 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. 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. Records kept since Iceland was settled show that Eyjafjallajökull volcano erupted in 920, 1612 or 1613, and 1821–23. Ash plume reached 11,000m in the air – reached the stratosphere. The eruption was explosive and much bigger then the eruption in Fimmvörðuháls. The Eyjafjallajökull eruption sequence of 2010, which lasted from January until May of that year, began with the onset of clusters of small earthquakes, and by early March the earthquake activity had increased in intensity and frequency. [54] The thick layer of ash that had fallen on some Icelandic pastures and farms at Raufarfell had become wet and compact, making it very difficult to continue farming, harvesting, or grazing livestock.[55]. Iceland’s Eyjafjallajökull (pronounced “AY-yah-fyah-lah-YOH-kuul”) Volcano roared to life on April 14, 2010, injecting billowing clouds of steam and volcanic ash into the atmosphere. By signing up for this email, you are agreeing to news, offers, and information from Encyclopaedia Britannica. 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. [64] In Scotland, the number of phone calls to health services for respiratory and eye irritation did not rise significantly. [44] Crustal expansion continued at Þorvaldseyri for two days after the eruption began, but was slowly decreasing whilst the volcanic activity was increasing. The closure resulted in 10 million passengers left stranded across the world. Mud, ice, and meltwater running off the volcano swelled local rivers and streams, especially the Markarfljót glacial river west of the volcano, which flooded farmland and damaged roads. In April 2010, Eyjafjallajökull, a volcano in southern Iceland, began spewing several kilometres of volcanic ash into the atmosphere.The cloud of ash forced the greatest airspace closure since World War II, cancelling nearly 100,000 flights and disrupting the travel plans of tourists and business travelers alike throughout northern Europe. About 20 countries closed their airspace to commercial jet traffic and it affected approximately 10 million travellers. The massive volcanic plumes released on the 14th of April 2010, covered almost the entirety of Northern Europe and forced more than 20 countries to close their airspace. The craters can be seen when hiking the Fimmvörðuháls trail as well as the lava field from the eruption called, Goðahraun. The eruption is thought to have begun on 20 March 2010, about 8 km (5 mi) east of the top crater of the volcano, on Fimmvörðuháls, the high neck between Eyjafjallajökull and the … [67][68] The presence and location of the plume depends upon the state of the eruption and the winds. At 250 ppm, death can occur within a few days. The view of the eruption from Þórólfsfel also includes a thermal imaging camera. 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. Its name is derived from an Icelandic phrase meaning “the island’s mountain glacier,” and the volcano itself lies beneath Eyjafjallajökull (Eyjafjalla Glacier). On March 21, fountains of lava began exiting through a 0.3-mile- (500-metre-) long vent in the ice-free Fimmvörduháls Pass, which separates the Eyjafjallajökull glacier from the larger glacier Mýrdalsjökull to the east. Two new craters were formed in this eruption called Magni and Móði after the sons of Thor, the Norse god of thunder. Instead, the police closed the road to Þórsmörk and the four-wheel-drive trail from Skógar village to the Fimmvörðuháls mountain pass, but these roads and trails were reopened on 29 March, though only for suitable four-wheel drive vehicles. [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. The erupted products were fragmented material, the majority fine-grained airborne tephra. The effects of the volcanic eru… Plume from Eyjafjallajökull volcano (tan streak) moving southeast over the North Atlantic Ocean, April 15, 2010. The 2010 eruption of Iceland's Eyjafjallajökull volcano had a huge impact on air travel, changing the assessment of risk by the aviation sector and catalyzing new lines of scientific investigation. 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. The eruption happened underneath an ice sheet. Fearing the damage to commercial aircraft and potential loss of life that could result from flying through the ash cloud, many European countries closed their national airspace and grounded flights for several days. 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. 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. The 2010 eruption caused the most widespread air travel disruption for 65 years. [36] This rise in water temperature was thought to be related to the eruption nearby and was affecting part of the Krossá drainage basin. Large-scale release of sulphur dioxide into the troposphere also poses a potential health risk, especially to people with pre-existing breathing disorders. The series of events that marked its latest eruption began on March 10, 2010 and continued for 23 days. 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. It was the highest level of air travel disruption since World War 2. The 2010 eruption of Eyjafjallajökull. Be on the lookout for your Britannica newsletter to get trusted stories delivered right to your inbox. 2.5.2010. When the second fissure appeared, the road was closed again because of the danger of flash floods, which could have developed if the fissure had opened near big ice caps or other snow reservoirs, but the road was again opened at around noon on 1 April. [65], Volcanic ash is a major hazard to aircraft. [3] By 21 May 2010, the second eruption phase had subsided to the point that no further lava or ash was being produced. [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. The Eyjafjallajökull eruption in 2010 had a huge impact on the aviation industry in Europe (Donovan & Oppenheimer, 2010). The volcano's explosive power was enough to inject ash directly into the jet stream. The Eyjafjallajökull eruption produced very little lava, but huge quantities of glass-rich ash which was ejected into the atmosphere. Iceland’s Eyjafjallajökull Volcano burst into life for the first time in 190 years on March 20, 2010. From 14–20 April, ash from the volcanic eruption covered large areas of Northern Europe. Iceland has several volcanoes and is situated on two tectonic plates – the North American plate and Eurasian plate. 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. Eyjafjallajökull volcano, beneath an extension of Mýrdalsjökull (Mýrdals Glacier), erupted in March 2010 for the first time since 1821. https://www.britannica.com/place/Eyjafjallajokull-volcano, NASA - Eruption of Eyjafjallajökull Volcano, Iceland, Global Volcanism Program - Eyjafjallajökull, Eyjafjallajökull volcano - Student Encyclopedia (Ages 11 and up). Craters in autumn. [46] Many witnesses were present while the new fissure opened. 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. The Eyjafjallajökull volcanic event has so far exhibited four different stages: an effusive stage followed by a brief quiescence, an explosive stage and a further quiescent stage. The eruption of Eyjafjallajökull volcano in 2010 lasted for 39 days, 14 April–23 May. The resulting meltwater flowed back into the erupting volcano, which created two specific phenomena: The rapidly vaporising water significantly increased the eruption's explosive power. About 30 minutes played in 18 seconds. In March 2010 a small eruption started close to the famoushiking trail Fimmvörðuháls. The first eruption phase ejected olivine basaltic andesite lava[11] several hundred metres into the air in what is known as an effusive eruption. Case study - eruption in a developed country: Eyjafjallajökull. This photo was taken at sunrise on a Saturday morning in October, by Ólafur Sigurjónsson who lives in Forsæti III nearby and has done frequent flying across the eruptive area. Although the volcanic eruptions were relatively small, the effects had a hugely debilitating impact on the European airline industry. About 500 farmers and their families had to escape from the areas of Fljótshlíð, Eyjafjöll, and Landeyjar were evacuated overnight (including a group of 30 schoolchildren and their three teachers[28][29] from Caistor Grammar School in England), and flights to and from Reykjavík and Keflavík International Airport were postponed, but on the evening of 21 March, domestic and international air traffic was allowed again. The second eruptive phase happened under 200 m (660 ft) of glacial ice. 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. [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. Published Mar 29, 2010 Land Volcanoes An ash-loaded eruption plume rose to more than 8 km (5.0 mi), deflected to the east by westerly winds. [8] Previous eruptions of Eyjafjallajökull have been followed by eruptions at its larger neighbour, Katla. Lava flows – 1000 degrees Calcius lava spewed 150m into the air. Additional localised disruption continued into May 2010. In these three cases the eruption of Eyjafjallajökull volcano occurred simultaneously with or was shortly followed by the eruption of Katla, a volcano located some 15.5 miles (25 km) to the east. This was 10–20 times the average discharge rate in the preceding flank eruption at Fimmvörðuháls. The Eyjafjallajökull volcano erupted in 920, 1612 and again from 1821 to 1823 when it caused a glacial lake outburst flood (or jökulhlaup). The April 2010 eruption of Eyjafjallajökull volcano (Figure 1), located on Iceland's southern coast, created unprecedented disruptions to European air traffic during 15–20 April, costing the aviation industry an estimated $250 million per day (see the related news item in this issue). The magma discharge rate was about 300 cubic metres per second (11,000 cu ft/s) or 750 t/s. From the initial eruptive activity at Eyjafjallajokull volcano in 2010, that was a lava producing eruption 20 March - 12 April, preceding the explosive eruption. The plume was driven southeast, across the North Atlantic Ocean to northern Europe, by the prevailing winds. The 2010 eruptions of Eyjafjallajökull were volcanic events at Eyjafjallajökull in Iceland which, although relatively small for volcanic eruptions, caused enormous disruption to air travel across western and northern Europe over an initial period of six days in April 2010. All ash dispersion models for this geographic region were produced by the VAAC in London. The direction of the jet stream was unusually stable at the time of the eruption's second phase, continuously southeast. [63] Six months later, the population living in the area had more respiratory symptoms than a control group from North Iceland, with no ashfall. Expanding gases from the rapid vaporization of ice started a series of moderate phreatomagmatic explosions (which result from the contact of water and magma) that sent a plume of steam and ash almost 7 miles (11 km) into the atmosphere. On April 14th 2010 the top crater in the center of the glacier of Eyjafjallajökull started erupting. [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'. Update on activity in Eyjafjallajökull 2010 Eruption in Eyjafjallajökull, Iceland. [45], A new fissure opened on 31 March, around 200 m (660 ft) north-west of the original fissure. The first phase of the 2010 eruption began late on the evening of 20 March at the Eyjafjallajökull. [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 eruption near Eyjafjallajökull persists into its second week, with continued lava fountaining and lava flows spilling into nearby canyons. 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. The initial visual report of the eruption was at 23:52 GMT, when a red cloud was observed at the volcano, lightening up the sky above the eruptive site. With a VEI (Volcanic Explosivity Index) of four, the 2010 eruption of Eyjafjallajökull was not one of the largest recorded eruptions, but the resulting damage was significant. Neither phase of the eruption was unusually powerful. With the first eruption occurring on March 20, 2010, there was little explosive activity but some production of … Ash ejection from this phase of the eruption was small, rising to no more than 4 km (2.5 mi) into the atmosphere. Additional localised disruption continued into May 2010. [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. From 14–20 April, ash from the volcanic eruption covered large areas of Northern Europe. Distributed by high velocity … 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. The eruption began on 20th March 2010 and ended 7 months later in October 2010. The initial eruption caused a 500 metre fissure in a nearby pass. 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. Fluoride poisoning can start in sheep at a diet with fluorine content of 25 ppm. 10:00", "Experimental Acute Sodium Fluoride Poisoning in Sheep: Renal, Hepatic, and Metabolic Effects", "Ash from Iceland Volcano Endangers Horses", "Ash Fall Causes South Iceland Farmers Serious Trouble", "Iceland's volcanic ash halts flights across Europe | World news", "Articles < Seismicity < Icelandic Meteorological office", "University of Iceland reports and scientists' quotes", "A survey of early health effects of the Eyjafjallajökull 2010 eruption in Iceland: a population-based study", "Health effects following the Eyjafjallajökull volcanic eruption: a cohort study", "Syndromic surveillance to assess the potential public health impact of the Icelandic volcanic ash plume across the United Kingdom, April 2010", "RAF grounds fighter jets after volcanic dust is found in engines | Home News | News", "Icelandair and the Eyjafjallajökull volcanic eruption in 2010", "Dirty thunderstorm shoots lightning from volcano", The eruption that changed Iceland forever, "Volcano could mean cooling, acid rain: 'Not like Pinatubo' so far, but potential is there", "Icelandic volcano won't affect the world's climate", "Geologist Ari Trausti Guðmundsson answers Iceland volcano questions | IceNews – Daily News", "APOD: 19 April 2010 – Ash and Lightning Above an Icelandic Volcano", "The Cataclysmic 1991 Eruption of Mount Pinatubo, Philippines", 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, Collection of Scientific Earth Observations and Models, Satellite evidence of hot lava flows from an Icelandic volcano (CIMSS Satellite Blog), Description of beginning of current eruption, (March 2010), Icelandic Met Office, Webpages and -links related to 2010 Eyjafjallajökull eruptions. 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