(1728–1791), grew famous because of the eldmessa ("fire sermon") that he delivered on 20 July 1783.
Lakagígar is the correct name, as Laki mountain itself did not erupt, as fissures opened up on each side of it.
Lakagígar is part of a volcanic system centered on the volcano Grímsvötn and including the volcano Thordarhyrna.
This outpouring of sulphur 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.
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.
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On 8 June 1783, a 25 km (15.5 mi) long fissure with 130 craters opened with phreatomagmatic explosions because of the groundwater interacting with the rising basalt magma.
Over a few days the eruptions became less explosive, Strombolian, and later Hawaiian in character, with high rates of lava effusion.
There is evidence that the Laki eruption weakened African and Indian monsoon circulations, leading to between 1 and 3 millimetres (0.04 and 0.12 in) less daily precipitation than normal over the Sahel of Africa, resulting in, among other effects, low flow in the River Nile.