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The 2011 eruption of Grímsvötn was a Plinian eruption of Grímsvötn, Iceland's most active volcano, which caused disruption to air travel in Northwestern Europe from 22–25 May 2011. The last eruption of Grímsvötn was in 2004, [ 2 ] with the previous most powerful eruptions in 1783, 1873 and 1902.
It is believed that the four eruptions between 1996 and 2011 could mark the beginning of an active period, during which an eruption in Grímsvötn in Vatnajökull may be expected every 2–7 years. Parallel volcanic activity in nearby Bárðarbunga is known to be associated with increased activity in Grímsvötn. Seismic activity has been ...
Pages in category "Grímsvötn" The following 4 pages are in this category, out of 4 total. ... 0–9. 2011 eruption of Grímsvötn; G. 1996 eruption of Gjálp; L. Laki
Grímsvötn has probably had more than 30 eruptions in the last 400 years, and produced around 55 cubic kilometres (13 cu mi) over the last 10,000 years. [1] Part of the East volcanic zone (EVZ) ) See Grímsvötn index , Vatnajökull index Grimsvötn ash cloud.
2011 eruption of Grímsvötn; N. 2011 Nabro eruption; 2011 North American heat wave; P. 2011–2012 Puyehue-Cordón Caulle eruption; T. Tropical Storm Rolf; 2011 ...
2011 eruption of Grímsvötn This page was last edited on 14 October 2020, at 01:21 (UTC). Text is available under the Creative Commons Attribution-ShareAlike 4.0 ...
The volcano also erupted in June about a mile south of Kilauea caldera, marking the first eruption in that region of the volcano in about 50 years. The last one took place in December 1974. The ...
The volcanic lake Grímsvötn was the source of a large jökulhlaup in 1996. [8] There was also a considerable but short-lived eruption of the volcano under these lakes at the beginning of November 2004. [9] On 21 May 2011 a volcanic eruption started in Grímsvötn in Vatnajökull National Park at around 19:00. [9]