Laki 690526 226148820 2008-07-17T01:15:21Z John 764861 /* Consequences in Europe */ repetition {{otheruses}} {{Infobox Mountain | Name=Laki | Photo=Lakagigar Iceland 2004-07-01.jpg|Laki | Caption= | Elevation= varies: canyon to 1725 [[m]] (5659 [[ft]]) | Location=[[Iceland]] | Prominence = | Coordinates = {{coor dms|64|03|53|N|18|13|34|W|type:mountain_region:CA}} | Topographic map = | Type=[[Fissure vent]]s | Age= | Last eruption=1783 | First ascent= | Easiest route= }} '''Laki''' or '''Lakagígar''' (''Craters of Laki'') is a [[Fissure vent|volcanic fissure]] situated in the south of [[Iceland]], not far from the canyon of [[Eldgjá]] and the small town [[Kirkjubæjarklaustur]], in [[Skaftafell National Park]]. Laki is part of a volcanic system, centering on the [[Grímsvötn]] volcano and including the [[Eldgjá]] canyon and [[Katla]] volcano, and lies between the [[glacier]]s of [[Mýrdalsjökull]] and [[Vatnajökull]], in an area of fissures which run in a south-west to north-east direction. In AD 934, the Laki system produced a very large [[volcanic]] [[eruption]], as a [[flood basalt]] in the Eldgjá eruption, which released {{convert|19.6|km3|cumi|lk=on}} of lava. In [[1783]]-[[1784]], the system erupted again, from the Laki fissure and the adjoining Grímsvötn volcano, pouring out an estimated {{convert|14|km3|cumi|1|abbr=on}} of [[basalt]] lava and clouds of poisonous [[fluorine]]/[[sulfur-dioxide]] compounds that killed over 50% of Iceland's livestock population, leading to famine which killed approximately 25% of the population. ==AD 934 eruption== The A.D. 934 Eldgjá eruption of the Laki system released {{convert|19.6|km3|cumi|1|abbr=on}} of [[flood basalt]], one of the largest [[volcanic]] [[eruption]]s on earth in historical times. ==1783 eruption== On [[8 June]] [[1783]], a [[fissure]] with 130 [[Volcanic crater|crater]]s opened with [[Phreatic eruption|phreatomagmatic]] explosions because of the groundwater interacting with the rising [[basalt]] [[magma]]. These are sometimes mistaken by non-volcanologists as being "plinian" but are not. Over a few days the eruptions became less explosive, [[Strombolian eruption|Strombolian]], and later [[Hawaiian eruption|Hawaiian]] in character, with high rates of lava [[effusion]]. This event is rated as [[Volcanic Explosivity Index|VEI]] 6 on the [[Volcanic Explosivity Index]], but the eight month emission of sulfuric aerosols resulted in one of the most important climatic and socially repercussive events of the last millennium.<ref>[Brayshay and Grattan, 1999; Demarée and Ogilvie, 2001]</ref> The eruption, also known as the [[Skaftáreldar]] ("Skaftá river fires") or Síðueldur, produced an estimated {{convert|14|km3|cumi|1|abbr=on}} of [[basalt]] lava, and the total volume of [[tephra]] emitted was {{convert|0.91|km3|cumi|1|abbr=on}}.<ref name="gvp">{{VNUM|1=1703-01=|2=Grímsvötn}}</ref> [[Lava fountain]]s were estimated to have reached heights of 800-1400 [[m]] (~2,600-4,600 [[ft]]). In [[Kingdom of Great Britain|Great Britain]], the summer of 1783 was known as the "sand-summer" due to ash fallout.<ref>[http://www.bbc.co.uk/timewatch BBC Timewatch: "Killer Cloud", broadcast 19 January 2007]</ref> The gases were carried by the convective eruption column to altitudes of about {{convert|15|km|mi|-1}}. The [[aerosol|aerosols]] built up caused a cooling effect in the [[Northern Hemisphere]]. The eruption continued until [[7 February]] [[1784]], but most of the lava was erupted in the first five months. Grímsvötn volcano, from which the Laki fissure extends, was also erupting at the time from 1783 until 1785. The outpouring of gases, including an estimated 8 million tons of [[fluorine]] and estimated 120 million tons of sulfur dioxide gave rise to what has since become known as the "Laki haze" across Europe. ===Consequences in Iceland=== The consequences for Iceland were catastrophic. An estimated 25% of the population<ref>Gunnar Karlsson (2000), ''Iceland's 1100 Years'', p. 181</ref> died in the famine and fluorine poisoning after the fissure eruptions ceased. Around 80% of sheep, 50% of cattle and 50% of horses died because of [[dental fluorosis|dental]] and [[skeletal fluorosis]] from the 8 million tons of fluorine that were released.<ref>[http://www.sciencemag.org/cgi/content/summary/306/5700/1278 VOLCANOLOGY: Iceland's Doomsday Scenario? - Stone 306 (5700): 1278 - Science<!-- Bot generated title -->]</ref><ref>[http://www.bbc.co.uk/timewatch BBC Timewatch: "Killer Cloud", broadcast 19 January 2007]</ref> The parish priest Jón Steingrímsson grew famous because of his ''eldmessa'' ("fire sermon"). The whole community of the small town of Kirkjubæjarklaustur was in church. At the same time the town was endangered by a lava stream. But while the people were in church, the lava stopped not far from town. :"This past week, and the two prior to it, more poison fell from the sky than words can describe: ash, volcanic hairs, rain full of sulfur and salt peter, all of it mixed with sand. The snouts, nostrils, and feet of livestock grazing or walking on the grass turned bright yellow and raw. All water went tepid and light blue in color and gravel slides turned gray. All the earth's plants burned, withered and turned gray, one after another, as the fire increased and neared the settlements."<ref>Rev. Jón Steingrímsson, ''Fires of the Earth, The Laki Eruption (1783-1784)'' ISBN 9979-54-244-6. Jón Steingrímsson's autobiography has been translated into English as ''A Very Present Help in Trouble: The Autobiography of the Fire-Priest'' ISBN 0-8204-5206-8.</ref> ===Consequences in Europe=== An estimated 122&nbsp;[[Teragram|Tg]] (120 million tons) of [[sulfur dioxide]] were emitted into the atmosphere: approximately equivalent to three times the total annual European industrial output in 2006, and also equivalent to a [[Mount Pinatubo]]-1991 eruption every three days.<ref>[http://www.bbc.co.uk/timewatch BBC Timewatch: "Killer Cloud", broadcast 19 January 2007]</ref> This outpouring of sulfur dioxide during unusual weather conditions caused a thick haze to spread across western Europe, resulting in many thousands of deaths throughout 1783 and the winter of 1784. The summer of 1783 was the hottest on record and a rare high pressure zone over Iceland caused the winds to blow to the south-east. The poisonous cloud drifted to [[Bergen]] in [[Norway]], then spread to [[Prague]] in the [[Bohemia|Province of Bohemia]] by [[17 June]], [[Berlin]] by [[18 June]], [[Paris]] by [[20 June]], [[Le Havre]] by [[22 June]], and to [[Great Britain]] by [[23 June]]. The fog was so thick that boats stayed in port, unable to navigate, and the sun was described as "blood coloured".<ref>[http://www.bbc.co.uk/timewatch BBC Timewatch: "Killer Cloud", broadcast 19 January 2007]</ref> <!-- needs a better citation --> Inhaling sulfur dioxide gas causes victims to choke as their internal soft tissue swells. The local death rate in [[Chartres]] was up by 5% during August and September, with over 40 dead. In Great Britain, the records show that the additional deaths were outdoor workers, and perhaps 2-3 times above the normal rate in Bedfordshire, Lincolnshire and the east coast. It has been estimated that 23,000 British people died from the poisoning in August and September. The haze also heated up causing severe thunderstorms with hailstones that were reported to have killed cattle until it dissipated in the autumn. This disruption then led to a most severe winter in 1784, where [[Gilbert White]] at [[Selborne]] in [[Hampshire]] reported 28 days of continuous frost. The extreme winter is estimated to have caused 8,000 additional deaths in the UK. In the spring thaw, Germany and Central Europe then reported severe flood damage.<ref>[http://www.bbc.co.uk/timewatch BBC Timewatch: "Killer Cloud", broadcast 19 January 2007]</ref> The meteorological impact of Laki resonated on, contributing significantly to several years of extreme weather in Europe. In France a sequence of extremes included a surplus harvest in 1785 that caused poverty for rural workers, accompanied by droughts, bad winters and summers, including a violent hailstorm in 1788 that destroyed crops. This in turn contributed significantly to the build up of poverty and famine that triggered the [[French Revolution]] in 1789. Laki was only a factor in a decade of climatic disruption, as [[Grímsvötn]] was erupting from 1783-1785 and a recent study of [[El Niño]] patterns also suggests an unusually strong El-Niño effect between 1789-93.<ref>Richard H. Grove, “Global Impact of the 1789–93 El Niño,” ''Nature'' 393 (1998), 318-319.</ref> ===Consequences in North America=== In [[North America]], the winter of 1784 was the longest and one of the coldest on record. It was the longest period of below-zero temperatures in [[New England]], the largest accumulation of snow in [[New Jersey]], and the longest freezing over of [[Chesapeake Bay]]. There was ice skating in [[Charleston Harbor]], a huge snowstorm hit the south, the [[Mississippi River]] froze at [[New Orleans]], and there was ice in the [[Gulf of Mexico]].<ref>Wood, C.A., 1992. "The climatic effects of the 1783 Laki eruption" in C. R. Harrington (Ed.), ''The Year Without a Summer?'' Canadian Museum of Nature, Ottawa, pp. 58– 77. </ref><ref>[http://perso.club-internet.fr/acatte/Iceland_Laki_in_english.htm volcanoes from Iceland : Laki<!-- Bot generated title -->]</ref> ===Other consequences=== There is also evidence that the Laki eruption had effects beyond Europe, with weakened [[Africa]]n and [[India]]n [[monsoon]] circulations, leading to precipitation anomalies of -1 to -3 mm (-0.04 to -0.12 inch) per day over the [[Sahel]] of Africa, resulting in, amongst other effects, low flow in the River [[Nile]].<ref>Luke Oman, Alan Robock, Georgiy L. Stenchikov, and Thorvaldur Thordarson, "High-latitude eruptions cast shadow over the African monsoon and the flow of the Nile" in ''Geophysical Research Letters'', Vol. 33, L18711, 2006, doi:10.1029/2006GL027665.</ref> It may also have exacerbated the [[Tenmei]] famine in Japan. ==Contemporary reports== [[Gilbert White]] recorded his perceptions of the event at [[Selborne]]: :The summer of the year 1783 was an amazing and portentous one, and full of horrible phaenomena; for besides the alarming meteors and tremendous thunder-storms that affrighted and distressed the different counties of this kingdom, the peculiar haze, or smokey fog, that prevailed for many weeks in this island, and in every part of Europe, and even beyond its limits, was a most extraordinary appearance, unlike anything known within the memory of man. By my journal I find that I had noticed this strange occurrence from June 23 to July 20 inclusive, during which period the wind varied to every quarter without making any alteration in the air. The sun, at noon, looked as blank as a clouded moon, and shed a rust- coloured ferruginous light on the ground, and floors of rooms; but was particularly lurid and blood-coloured at rising and setting. All the time the heat was so intense that butchers' meat could hardly be eaten on the day after it was killed; and the flies swarmed so in the lanes and hedges that they rendered the horses half frantic, and riding irksome. The country people began to look with a superstitious awe, at the red, louring aspect of the sun; [...]<ref> Gilbert White - ''The Natural History and Antiquities of Selborne'', Letter LXV (1789).</ref> [[Benjamin Franklin]] recorded his observations in a 1784 lecture: :During several of the summer months of the year 1783, when the effect of the sun's rays to heat the earth in these northern regions should have been greater, there existed a constant fog over all Europe, and a great part of North America. This fog was of a permanent nature; it was dry, and the rays of the sun seemed to have little effect towards dissipating it, as they easily do a moist fog, arising from water. They were indeed rendered so faint in passing through it, that when collected in the focus of a burning glass they would scarce kindle brown paper. Of course, their summer effect in heating the Earth was exceedingly diminished. Hence the surface was early frozen. Hence the first snows remained on it unmelted, and received continual additions. Hence the air was more chilled, and the winds more severely cold. Hence perhaps the winter of 1783-4 was more severe than any that had happened for many years. : The cause of this universal fog is not yet ascertained [...] or whether it was the vast quantity of smoke, long continuing, to issue during the summer from [[Hekla|Hecla]] in Iceland, and that other volcano which arose out of the sea near that island, which smoke might be spread by various winds, over the northern part of the world, is yet uncertain.<ref>Benjamin Franklin - "Meteorological imaginations and conjectures" in ''Mem. Lit. Philos. Soc. Manchester'' 2, 373–377 (1784).</ref> ''(It should be noted that, according to [[Hekla|current records, Hekla]] did not erupt in 1783, its previous eruption was in 1766. The Laki fissure eruption was 45 miles<ref>{{convert|45|mi|km}}</ref> to the east and the [[Grímsvötn]] volcano was erupting circa 75 miles<ref>{{convert|75|mi|km}}</ref> north east. Additionally [[Katla]], only 31 miles<ref>{{convert|31|mi|km}}</ref> south east, was still renowned after its spectacular eruption 28 years earlier in 1755.)'' The Reverend Sir John Cullum of [[Bury St Edmunds]] [[Suffolk]] [[UK]] recorded on the 23rd June 1783, the same date that Gilbert White noted the beginning of the unusual atmospheric phenomena, in a letter to [[Joseph Banks|Sir Joseph Banks]], then President of [[The Royal Society]] :...‘about six o’clock, that morning, I observed the air very much condensed in my chamber-window; and, upon getting up, was informed by a tenant that finding himself cold in bed, about three o’clock in the morning, he looked out at his window, and to his great surprise saw the ground covered with a white frost: and I was assured that two men at Barton, about three miles off, saw in some shallow tubs, ice of the thickness of a crown-piece.’<ref name="J.C.">{{cite web | last = Bury | first = Free Press | title = The remarkable frost of June. |url=http://www.buryfreepress.co.uk/peep-into-the-past/The-remarkable-frost-of-June.1885164.jp | accessdate = 2008-06-20 }}</ref> Sir John goes on to describe the effect of this ‘frost’ on trees and crops: :‘The aristae<ref>a bristlelike structure or appendage, the ear of barley</ref> of the barley, which was coming into ear, became brown and withered at their extremities, as did the leaves of the oats; the rye had the appearance of being mildewed; so that the farmers were alarmed for those crops…The larch, Weymouth pine, and hardy Scotch fir, had the tips of their leaves withered’.<ref name="J.C."/> Sir John’s vegetable garden did not escape either, for he noted that they appeared ‘exactly as if a fire had been lighted near them, that had shrivelled and discoloured their leaves’. ==See also== * [[Geography of Iceland]] * [[Glaciers of Iceland]] * [[Glacial lake outburst flood]] * [[Iceland plume]] * [[Iceland hotspot]] * [[Lakes of Iceland]] * [[List of islands off Iceland]] * [[List of volcanoes in Iceland]] * [[Plate tectonics]] * [[Rivers of Iceland]] * [[Volcanoes of Iceland]] * [[Waterfalls of Iceland]] * [[Year Without a Summer]] ==References== <div class="references-small"><references/></div> ==Further reading== *Brayshay, M and Grattan, J. - "Environmental and social responses in Europe to the 1783 eruption of the Laki fissure volcano in Iceland: a consideration of contemporary documentary evidence" in Firth, C. R. and McGuire, W. J. (eds) ''Volcanoes in the Quaternary''. Geological Society, London, Special Publication 161, 173-187, 1999 *Grattan, J., Brayshay, M. and Sadler, J. - "Modelling the distal impacts of past volcanic gas emissions: Evidence of Europe-wide environmental impacts from gases emitted during the eruption of Italian and Icelandic volcanoes in 1783" in ''Quaternaire'', 9, 25-35. 1998. *Grattan, D., Schütenhelm, R. and Brayshay, M. - "Volcanic gases, environmental crises and social response" in Grattan, J. and Torrence, R. (eds) ''Natural Disasters and Cultural Change'', Routledge, London 87-106. 2002. *Grattan, J.P. and Brayshay, M.B. - "[http://www.questia.com/PM.qst?a=o&d=5000338532&er=deny An Amazing and Portentous summer: Environmental and social responses in Britain to the 1783 eruption of an Iceland Volcano]" in ''The Geographical Journal'' 161(2), 125-134. 1995. * Richard B. Stothers - "[http://pubs.giss.nasa.gov/abstracts/1996/Stothers_2.html The great dry fog of 1783]" in ''Climatic Change'', 32, 79–89, 1996. * "The Summer of Acid Rain", ''Economist'', December 19, 2007. * Thorvaldur Thordarson and Stephen Self - "[http://oro.open.ac.uk/5099/ Atmospheric and environmental effects of the 1783–1784 Laki eruption]; a review and reassessment" in ''J. Geophys. Res.'', 108, D1, 4011, doi:10.1029/2001JD002042, 2003. == External links== *[http://perso.club-internet.fr/acatte/Iceland_Laki_in_english.htm Photos and information] *[http://volcano.und.edu/vwdocs/volc_images/europe_west_asia/laki.html Information about the volcanism at Laki] *[http://www.umhverfisstofnun.is/media/fraedsluefni/Lakagigar_enska.pdf Lakagígar] *[http://morgue.anglicansonline.org/051106/ A meditation on Jón Steingrímsson] from [[Anglicans Online]] *[http://www.esc.cam.ac.uk/ivhhn/members/people/grattan.html Dr John Grattan at International Volcanic Heath Hazard Network] *[http://www.agu.org/meetings/cc02babstracts/Grattan-p.pdf A Sulphurous Stench: Illness and Death in Europe Following the Eruption of the Laki Fissure] {{coor title dms|64|03|53|N|18|13|34|W|region:IS_type:landmark}} [[Category:1783 disasters]] [[Category:Flood basalts]] [[Category:History of Iceland]] [[Category:Mountains of Iceland]] [[Category:Volcanoes of Iceland]] [[Category:VEI-6 volcanoes]] [[Category:Natural disasters in England|Laki haze]] [[Category:Fissure vents]] [[af:Laki]] [[ca:Volcà Laki]] [[da:Laki]] [[de:Laki-Krater]] [[et:Laki]] [[fr:Laki]] [[is:Lakagígar]] [[lt:Lakis]] [[nl:Laki]] [[ja:ラキ火山]] [[no:Laki]] [[nn:Laki]] [[pl:Laki]] [[ru:Лаки (вулкан)]] [[sr:Кратер Лаки]] [[fi:Lakagigar]] [[sv:Laki]] [[ta:லாக்கி]] [[uk:Лакі]]