Katla eruption 1918
|Elevation||1,512 m (4,961 ft)|
|Listing||List of volcanoes in Iceland|
Katla (Icelandic pronunciation: [ˈkʰahtla] ( listen)) is a large volcano in southern Iceland. It is very active; twenty eruptions have been documented between 930 and 1918, at intervals of 13–95 years. It has not erupted violently for 95 years, although there may have been small eruptions that did not break the ice cover, including ones in 1955 and 1999.
Prior eruptions have had a Volcanic Explosivity Index (VEI) of between 4 and 6 on a scale of 0 to 8. In comparison, the Eyjafjallajökull 2010 eruption had a VEI4. The bigger VEI6 eruptions are comparable to Mount Pinatubo's 1991 eruption.
Geography and features 
Katla is one of the largest volcanoes in Iceland. It is situated to the north of Vík í Mýrdal and to the east of the smaller glacier Eyjafjallajökull. Its peak reaches 1,512 metres (4,961 ft) and is partially covered by the Mýrdalsjökull glacier. The system has an area of 595 km2 (230 sq mi). The Eldgjá canyon is part of the same volcanic system.
The caldera of the Katla volcano has a diameter of 10 km (6 mi) and is covered with 200–700 metres (660-2,300 ft) of ice. The volcano normally erupts every 40–80 years. The flood discharge at the peak of an eruption in 1755 has been estimated at 200,000–400,000 m3/s (7.1-14.1 million cu ft/sec), comparable to the combined average discharge of the Amazon, Mississippi, Nile, and Yangtze rivers (about 266,000 m3/s (9.4 million cu ft/sec)).
Prehistoric activity 
It is thought that Katla is the source of Vedde Ash, more than 6 to 7 cubic kilometers (1.4 to 1.7 cu mi) of tephra dated to 10,600 years BP found at a number of sites including Vedde in Denmark, Norway, Scotland and North Atlantic cores.
Historic activity 
Sixteen eruptions have been recorded for Katla since 930. The last major eruption started on 12 October 1918 and lasted for 24 days. It was likely a VEI5 level eruption. The 1918 eruption resulted in extending the southern coast by 5 km due to laharic flood deposits. Its present dormancy is among the longest in known history.
Major eruptions occurred in :
Most of these eruptions resulted in glacial floods. The severe fissure eruption in 934 was one of the largest lava eruptions in the past 10,000 years. Before the Hringvegur (Iceland's Ring Road) was constructed in 1974, people feared traversing the plains in front of the volcano because of the frequent jökulhlaup (or glacier bursts) and the deep river crossings. Especially dangerous was the glacier outburst that followed the eruption of 1918.
Present day activity 
Katla has been showing signs of unrest since 1999, and geologists have concerns that it might erupt in the near future. Particularly, monitoring has been intensified following the March 2010 eruptions of a smaller neighbouring volcano, the Eyjafjallajökull glacier. The eruption of this nearby long-dormant volcano in March and April 2010 prompted fears among some geophysicists that it might trigger an eruption at the larger and more dangerous Katla. In the past 1,000 years, all three known eruptions of Eyjafjallajökull have triggered subsequent Katla eruptions.
Following the 2010 Eyjafjallajökull eruptions, on 20 April 2010 Icelandic President Ólafur Grímsson said "the time for Katla to erupt is coming close ... we [Iceland] have prepared ... it is high time for European governments and airline authorities all over Europe and the world to start planning for the eventual Katla eruption".
Increased earthquake activity has been noticed on Katla since the eruption at Eyjafjallajökull, but no other signs of an imminent eruption have been observed. These quakes are located mainly on the northwestern rim of the caldera. On 9 October 2010, a sudden rise in harmonic tremor was observed in the stations around Katla, a sign of a possible impending eruption.
As of 2010[update], volcanologists are continuing to monitor Katla, aware that any eruption from Katla following an eruption from Eyjafjallajökull has historically occurred within months of the latter. The Icelandic Meteorological Office updates its website with reports of quakes both at Eyjafjallajökull and Katla.
In June 2011, harmonic tremor was again detected at Katla volcano. A few days later, an earthquake swarm took place in the caldera, indicating magma movement inside the volcano, leading to increased fears of an eruption in the near future.
On 8 and 9 July another spike in harmonic tremors occurred. Icelandic media reported a small subglacial eruption might have started. On the morning of 9 July a glacier flood was reported in the river Múlakvísl, later also in the river Skálm. The bridge across Múlakvísl was destroyed as well as other parts of the road, Route 1, on the Icelandic ring road. Helicopter pilots flying over the glacier also reported cracks in the glacier, suggesting a large meltdown of the glacier on the south-eastern rim of the Katla crater.
2011 Eruption 
A small eruption of Katla took place on 8 July 2011. After a harmonic tremor was detected, cracks formed on the Glacier as well as a cauldron. The event produced a jökulhlaup that destroyed a road bridge. These events have been linked to a small eruption from Katla.
See also 
- "Katla Volcano". Institute of Earth Sciences. University of Iceland. Retrieved 2010-03-12.
- 1999 Eruption, jökulhlaup
- "Katla". Global Volcanism Program, Smithsonian Institution. http://www.volcano.si.edu/world/volcano.cfm?vnum=1702-03%3D. Retrieved 2010-03-26.
- Gudmundsson, Magnús T.; Thórdís Högnadóttir (January 2007). "Volcanic systems and calderas in the Vatnajökull region, central Iceland: Constraints on crustal structure from gravity data". Journal of Geodynamics 43 (1): 153–169. Bibcode:2007JGeo...43..153G. doi:10.1016/j.jog.2006.09.015.
- Katla - Nordic Names Wiki - Name Origin, Meaning and Statistics
- Mangerud , J., Lie, S.V., Furned, H., Kristiansen, I.L., Lømo, L. (1984) A Younger Dryas Ash Bed in Western Norway, and Its Possible Correlations with Tephra in Cores from the Norwegian Sea and the North Atlantic. Quaternary Research 21 85-104
- Grönvold, K.; Oskarsson N., Johnsen S.J., Clausen H.B., Hammer C.U., Bond G. and Bard E. (1995). "Ash layers from Iceland in the Greenland GRIP ice core correlated with oceanic and land sediments". Earth Planet Sci Lett 135: 149–155. Bibcode:1995E&PSL.135..149G. doi:10.1016/0012-821X(95)00145-3.
- Árni Hjartarson (2003), "Postglacial Lava Production in Iceland", in Árni Hjartarson, PhD-thesis, Geological Museum, University of Copenhagen, pp. 95–108
- Katla Volcano News
- Soosalu, Heidi. "Katla seismicity". Institute of Earth Sciences. University of Iceland. Retrieved 2010-03-12.
- "Hard to Predict How Long Iceland Eruption Will Last". Iceland Review (Iceland). 21 March 2010. Retrieved 21 March 2010.
- Volcano erupts in south Iceland BBC online news. Retrieved 21 March 2010.
- Boyes, Roger (2010-03-21). "Iceland prepares for second, more devastating volcanic eruption". Times Online. Retrieved 2010-03-22.
- "Icelandic Volcano May Cause Bigger Eruption". Reuters. 2010-03-22. Retrieved 2010-04-20.
- BBC Newsnight interview with President Grímsson of Iceland, 20 April 2010
- Frímann, Jón. "Sudden rise in harmonic tremors around Katla and Eyjafjallajökull". Iceland Volcano and Earthquake Blog. Retrieved 30 December 2010.
- Iceland Meteorological office - Earthquakes Mýrdalsjökull, Iceland
- Frímann, Jón (17 June 2011). "Earthquake swarm in Katla volcano". Iceland Volcano and Earthquake Blog. Retrieved 18 October 2011.
- "Hlaup hafið í Múlakvísl". Morgunblaðið (in Icelandic). 9 July 2011. Retrieved 18 October 2011.
- "Sjá sprungur í jöklinum". Morgunblaðið (in Icelandic). 9 July 2011. Retrieved 18 October 2011.
- "Katla volcano in Iceland remains dormant". IceNews. 9 July 2011.
|Wikimedia Commons has media related to: Katla|
- Volcanism 1
- University of Iceland's Institute of Earth Sciences page about Katla
- Webcams from Iceland, including Katla
- Katla: preparedness for tourists
- Icelandic Meteorological Office: Katla status
- Constantly updating map of earthquakes in Mýrdalsjökull