Laki

Template:Short description {{#invoke:other uses|otheruses}} Template:Infobox mountain

Laki ({{#invoke:IPA|main}}) or Lakagígar ({{#invoke:IPA|main}}, Craters of Laki) is a volcanic fissure in the western part of Vatnajökull National Park, Iceland, not far from the volcanic fissure of Eldgjá and the small village of Kirkjubæjarklaustur. The fissure is properly referred to as Lakagígar, while Laki is a mountain that the fissure bisects. Lakagígar is part of a volcanic system centered on the volcano Grímsvötn and including the volcano Þórðarhyrna.<ref name="gvp">Template:Cite gvp</ref><ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref><ref>Template:Cite journal</ref> It lies between the glaciers of Mýrdalsjökull and Vatnajökull, in an area of fissures that run in a southwest to northeast direction.

The system erupted violently over an eight-month period between June 1783 and February 1784 from the Laki fissure and the adjoining volcano Grímsvötn. It poured out an estimated 42 billion tonnes or Template:Convert of basalt lava as well as clouds of poisonous hydrofluoric acid and sulfur dioxide compounds that contaminated the soil, leading to the death of over 50% of Iceland's livestock population, and the destruction of the vast majority of all crops. This led to a famine which then killed at least a fifth<ref name="1783–1784 Laki eruption"/> of the island's human population, although some have claimed a quarter.<ref>Gunnar Karlsson (2000), Iceland's 1100 Years, p. 181.</ref>

The Laki eruption and its aftermath caused a drop in global temperatures, as 120 million tonnes of sulfur dioxide was spewed into the Northern Hemisphere. This caused crop failures in Europe and may have caused droughts in North Africa and India.

1783 eruptionEdit

Template:Infobox eruption On 8 June 1783, a Template:Cvt fissure of at least 130 vents opened with phreatomagmatic explosions because of the groundwater interacting with the rising basalt magma.<ref name="econ" /> Over a few days the eruptions became less explosive, Strombolian, and later Hawaiian in character, with high rates of lava effusion. This event is rated as 4 on the Volcanic Explosivity Index,<ref name="Laki1783GVP">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> but the eight-month emission of sulfuric aerosols resulted in one of the most important climatic and socially significant natural events of the last millennium.<ref>Brayshay and Grattan, 1999; Demarée and Ogilvie, 2001.</ref><ref name="econ">Template:Cite news</ref>

The eruption, also known as the {{#invoke:Lang|lang}} {{#invoke:IPA|main}} ("Skaftá fires") or Síðueldur {{#invoke:IPA|main}} produced an estimated Template:Convert of basalt lava, and the total volume of tephra emitted was Template:Convert.<ref name="gvp2">Template:Cite gvp</ref> Lava fountains were estimated to have reached heights of Template:Convert. The gases were carried by the convective eruption column to altitudes of about Template:Convert.<ref name="1783–1784 Laki eruption">Template:Cite journal</ref>

The eruption continued until 7 February 1784, but most of the lava was ejected in the first five months. One study states that the event "occurred as ten pulses of activity, each starting with a short-lived explosive phase followed by a long-lived period of fire-fountaining".<ref name="BCS">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> Grímsvötn volcano, from which the Laki fissure extends, also erupted at the time, from 1783 until 1785. The outpouring of gases, including an estimated 8 million tonnes of fluorine and an estimated 120 million tonnes of sulfur dioxide, gave rise to what has since become known as the "Laki haze" across Europe.<ref name="1783–1784 Laki eruption"/>

Consequences in IcelandEdit

The consequences for Iceland, known as the {{#invoke:Lang|lang}} {{#invoke:IPA|main}} (mist hardships), were disastrous.<ref>Template:Cite news</ref> An estimated 20–25% of the population died in the famine after the fissure eruptions ensued. (Some sources specify a death toll of between 9,000 and 9,500 people.)<ref name=EBI2011 /><ref name="news.bbc.co.uk">Template:Cite news</ref> Approximately 80% of sheep (190,500 head), 50% of cattle (11,500 head) and 50% of horses (28,000 head) died because of dental fluorosis and skeletal fluorosis from the 8 million tons of fluorine that were released.<ref name=EBI2011 /><ref name="bbc.co.uk">Template:Cite episode</ref><ref>Template:Cite magazine</ref> The livestock deaths were primarily caused by eating contaminated grass, while humans deaths were mostly from the subsequent famine.<ref name="news.bbc.co.uk"/>

The parish minister and provost of Vestur-Skaftafellssýsla, Jón Steingrímsson (1728–1791), grew famous for the {{#invoke:Lang|lang}} {{#invoke:IPA|main}} ("fire mass") that he delivered on 20 July 1783. The church farm of Kirkjubæjarklaustur was endangered by a branch of the lava flow that halted not far from the farm while the Rev. Jón and his parishioners were worshipping in the church. The spot at which the lava diverted away from the church became known thereafter as {{#invoke:Lang|lang}} {{#invoke:IPA|main}} ("Fire Mass Point").

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File:Laki fissure (2).jpg

Center of the Laki fissure

Consequences in monsoon regionsEdit

There is evidence that the Laki eruption weakened African and Indian monsoon circulations, leading to between Template:Convert less daily precipitation than normal over the Sahel of Africa, resulting in, among other effects, low flow in the River Nile.<ref name="grl" /> The resulting famine that afflicted Egypt in 1784 cost it roughly one-sixth of its population.<ref name="grl">Template:Cite journal</ref><ref name="sdaily">Template:Cite news</ref> The eruption was also found to have affected South Arabia and the already ongoing Chalisa famine in India.<ref name="sdaily" /><ref>Template:Cite journal</ref>

Consequences in East AsiaEdit

The Great Tenmei famine of 1782–1788 in Japan may have been worsened by the Laki eruption. In the same year, Mount Asama erupted in Japan (Tenmei eruption).<ref name="tenmei">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> The eruption may have affected a drought in eastern China.<ref>Template:Cite journal</ref>

Consequences in EuropeEdit

File:Laki, Iceland 2012-07 D.JPG

Laki in July 2012

An estimated 120,000,000 tonnes of sulfur dioxide was emitted, about three times the total annual European industrial output in 2006 (but delivered to higher altitudes, hence its persistence), and equivalent to six times the total 1991 Mount Pinatubo eruption.<ref name="bbc.co.uk"/><ref name="1783–1784 Laki eruption" /> 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 the remainder of 1783 and the winter of 1784.Template:Citation needed

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.<ref name="bbc.co.uk"/> The poisonous cloud drifted to Bergen in Denmark–Norway, then spread to Prague in the Kingdom of Bohemia (now the Czech Republic) by 17 June, Berlin by 18 June, Paris by 20 June, Le Havre by 22 June, and Great Britain by 23 June. The fog was so thick that ships stayed in port, unable to navigate, and the sun was described as "blood coloured".<ref name="bbc.co.uk"/>

Inhaling sulfur dioxide gas causes victims to choke as their internal soft tissues swell – the gas reacts with the moisture in the lungs and produces sulfurous acid.<ref name="elmhurst">{{#invoke:citation/CS1|citation |CitationClass=web }}</ref> The local death rate in Chartres was up by 5% during August and September, with more than 40 dead. In Great Britain, the east of England was most affected. The records show that the additional deaths were among outdoor workers; the death rate in Bedfordshire, Lincolnshire, and the east coast was perhaps two or three times the normal rate. It has been estimated that 23,000 British people died from the poisoning.<ref>Template:Cite news</ref>

The weather became very hot, causing severe thunderstorms with large hailstones that were reported to have killed cattle,<ref>{{#invoke:citation/CS1|citation |CitationClass=web }} Quotes reports from the Newcastle Courant and Cumberland Pacquet newspapers.</ref> until the haze dissipated in the autumn. The winter of 1783–1784 was very severe;<ref>{{#invoke:citation/CS1|citation |CitationClass=web }} Quotes reports from the Newcastle Courant and Cumberland Pacquet newspapers.</ref> the naturalist Gilbert White in Selborne, Hampshire, reported 28 days of continuous frost. The extreme winter is estimated to have caused 8,000 additional deaths in the UK. During the spring thaw, Germany and Central Europe reported severe flood damage.<ref name="bbc.co.uk"/> This is considered part of a volcanic winter.<ref name="Wood58-57">Template:Cite book</ref>

The meteorological impact of Laki continued, contributing significantly to several years of extreme weather in Europe. In France, the sequence of extreme weather events included a failed harvest in 1785 that caused poverty for rural workers, as well as droughts, bad winters and summers. These events contributed significantly to an increase in poverty and famine that may have contributed to the French Revolution in 1789.<ref name="Wood58-57"/> Laki was only one factor in a decade of climatic disruption, as Grímsvötn was erupting from 1783 to 1785, and there may have been an unusually strong El Niño effect from 1789 to 1793.<ref>Template:Cite journal</ref><ref>Template:Cite journal</ref>

Consequences in North AmericaEdit

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, with the largest accumulation of snow in New Jersey, and the longest freezing over of Chesapeake Bay. At the time, the capital of the United States was situated on the Chesapeake at Annapolis, Maryland; the weather delayed Congressmen who were traveling there to vote for the Treaty of Paris, which formally ended the American Revolutionary War. A huge snowstorm hit the South; the Mississippi River froze at New Orleans and there were reports of ice floes in the Gulf of Mexico.<ref name="Wood58-57"/><ref>{{#invoke:citation/CS1|citation |CitationClass=web }}</ref>

Contemporaneous reportsEdit

File:Kirkjubaejarklaustur.jpg

Kirkjubaejarklaustur, an important church farm in South Iceland, was the home of the Rev. Jón Steingrímsson (1728–1791), who left contemporary eyewitness accounts of the effects of the eruption and its aftermath. Today, Kirkjubæjarkaustur is a small village.

Gilbert White recorded his perceptions of the event at Selborne, Hampshire, England:

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Benjamin Franklin recorded his observations in America in a 1784 lecture:

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According to contemporary records, Hekla did not erupt in 1783; its previous eruption was in 1766. The Laki fissure eruption was Template:Convert east and the Grímsvötn volcano was erupting about Template:Convert northeast. Katla, only Template:Convert southeast, was still renowned after its spectacular eruption 28 years earlier in 1755.

Sir John Cullum of Bury St Edmunds, Suffolk, England, recorded his observations on 23 June 1783 (the same date on which Gilbert White noted the onset of the unusual atmospheric phenomena), in a letter to Sir Joseph Banks, then President of the Royal Society:

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Sir John goes on to describe the effect of this "frost" on trees and crops:

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