Laki is part of a volcanic system, centering on the Grímsvötn volcano and including the Eldgjá canyon and Katla volcano, and lies between the glaciers 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 volcaniceruption, as a flood basalt in the Eldgjá eruption, which released 19.6 km³ (4.7 mi³) of lava.
In 1783-1784, the system erupted again, from the Laki fissure and the adjoining Grímsvötn volcano, spewing 15 km³ (3.6 mi³) of basalt lava and clouds of poisonous fluorine/sulfur-dioxide compounds that killed over 50% of livestock, leading to famine killing 25%-33% of the population.
Contents
1AD 934 eruption
21783 eruption
2.1Consequences in Iceland
2.2Consequences in Europe
2.3Consequences in North America
2.4Other consequences
3Contemporary reports
4See also
5References
6Further reading
7External links
AD 934 eruption
The Laki system produced the biggest volcaniceruption on earth in historical times, in the form of a flood basalt, during the Eldgjá eruption A.D. 934, which released 19.6 km³ (4.7 mi³) of lava.
1783 eruption
On 8 June1783, a fissure with 130 craters opened explosively at first because of the groundwater interacting with the rising basaltmagma. Over time, the eruptions became less explosive, with the style changing from Plinian to Strombolian, and later to Hawaiian with high rates of lava effusion. This event is rated as VEI 4 on the Volcanic Explosivity Index, but the eight month emission of sulphuric aerosols resulted in one of the most important climatic and socially repercussive events of the last millennium.[1]
The eruption, also known as the Skaftáreldar ("Skaftá river fires") or Sîðueldur, produced about 15 km³ (3.6 mi³) of basalt lava, and the total volume of tephra emitted was 0.91 km3.[2]Lava fountains were estimated to have reached heights of 800-1400 m (~2,600-4,600 ft). In the United Kingdom, the summer of 1783 was known as the "sand-summer" due to ash fallout.[3] The gases were carried by the convective eruption column to altitudes of about 15 km. The aerosols built up caused a cooling effect in the Northern Hemisphere.
The eruption continued until 7 February1784, 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 8 million tons of fluorine and 120 million tons of sulphur dioxide gave rise to what has since become known as the "Laki haze" across Europe.
Consequences in Iceland
The consequences for Iceland were catastrophic, approximately 25-33% of the population died in the famine of 1783 to 1784 after the fissure eruptions ceased. Around 80% of sheep, 50% of cattle and 50% of horses died because of fluorosis from the 8 million tons of fluorine that were released.[4][5]
The parish priest Jón Steingrimsson 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 the another, as the fire increased and neared the settlements."[6]
Consequences in Europe
An estimated 122 Tg (120 Million tons) of sulphur dioxide was 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.[7] This outpouring of sulphur dioxide during unusual weather conditions caused a thick sulphurous 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 west. The poisonous cloud drifted to Bergen in Norway, then spread to Prague in the Czech Republic by 17 June, Berlin by 18 June, Paris by 20 June, Le Havre by 22 June, and to the United Kingdom by 23 June. The fog was so thick that boats stayed in port, unable to navigate, and the sun was described as "blood coloured".[8]
Inhaling sulphurous 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 the UK 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 thunder storms with hailstones that were reported to have killed cattle until it disipated in the autumn. This disruption then led to a most severe winter in 1784, where Gilbert White at Selborne in Hampshire reported with 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.[9]
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 Grimsvotn was erupting from 1783-1785 and a recent study of El Niño patterns also suggests an unusually strong El-Niño effect between 1789-93.[10]
There is also evidence that the Laki eruption had effects beyond Europe, with weakened African and Indianmonsoon 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.[13]
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; [...][14]
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 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.[15](It should be noted that, according to current records, Hekla did not erupt in 1783, its previous eruption was in 1766. The Laki fissure eruption was 45 miles to the east and the Grimsvotn volcano was erupting circa 75 miles north east. Additionally Katla, only 31 miles south east, was still renowned after its spectacular eruption 28 years earlier in 1755.)
^ Rev. Jón Steingrímsson, Fires of the Earth, The Laki Eruption (1783-1784)ISBN 9979-54-244-6. Steingrimsson's autobiography has been translated into English as A Very Present Help in Trouble: The Autobiography of the Fire-PriestISBN 0-8204-5206-8.
^ Richard H. Grove, “Global Impact of the 1789–93 El Niño,” Nature 393 (1998), 318-319.
^ 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.
^ 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.
^ Gilbert White - The Natural History and Antiquities of Selborne, Letter LXV (1789).
^ Benjamin Franklin - "Meteorological imaginations and conjectures" in Mem. Lit. Philos. Soc. Manchester 2, 373–377 (1784).
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.
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