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  • 31. Web-pages related to the Grímsvötn eruption 2011

    Of interest - Bárðarbunga Reduction of the accesscontrolled area around Holuhraun lava field END OF ERUPTION declaredby the Scientific Board Location map (detailed)around the new lava field Bárðarbunga earthquakes3D interactive model Thickness and volumeestimate from January 1st Comparing /earthquakes-and-volcanism/articles/nr/2220
  • 32. Ash cloud extending to Europe

    aviation authorities consider the ash cloud to be an hazard to aviation, are advised to examine the homepage of the Volcano Advisory Centre in London. Click on the link "Issued graphics" above the map, and choose the most recent map. For more news, click 2010. News 2023 /about-imo/news/nr/1873
  • 33. Ash plume and lightnings

    active volcano. It last erupted in 2004 and the current eruption is in a similar location. Flash floods south of the volcano often occur associated with eruptions, but can also happen in between eruptions. The latest such flood occurred in October 2010, so a big flood currently appears unlikely. The MODIS satellite picture taken around 5 o'clock this morning shows the plume; at sunrise the plume /about-imo/news/nr/2177
  • 34. Ash cloud extending to Europe

    aviation authorities consider the ash cloud to be an hazard to aviation, are advised to examine the homepage of the Volcano Advisory Centre in London. Click on the link "Issued graphics" above the map, and choose the most recent map. For more news, click 2010. News 2023 /about-imo/news/2010/nr/1873
  • 35. Ash cloud extending to Europe

    aloft are forecast for the weekend. Those who want to follow the areas, within which aviation authorities consider the ash cloud to be an hazard to aviation, are advised to examine the homepage of the Volcano Advisory Centre in London. Click on the link "Issued graphics" above the map, and choose the most recent map. For more news, click 2010 /about-imo/news/nr/1873/
  • 36. Ash cloud extending to Europe

    aloft are forecast for the weekend. Those who want to follow the areas, within which aviation authorities consider the ash cloud to be an hazard to aviation, are advised to examine the homepage of the Volcano Advisory Centre in London. Click on the link "Issued graphics" above the map, and choose the most recent map. For more news, click 2010 /about-imo/news/2010/nr/1873/
  • 37. VI_2009_006_tt

    lake in a volcanic caldera in the interior of the Vatnajökull ice cap (Björns- son, 1988). Jökulhlaups from Grímsvötn have been known since at least the fourteenth century (Þórarinsson, 1939, 1974). In the beginning of the twentieth century there were about ten years between outbursts but the floods diminished with time and became more frequent. After a catastrophic, rapidly rising flood caused /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf
  • 38. IMO at the Arctic Circle Assembly 2017

    the USA, the European Space Agency (ESA) and China.Ingvar Kristinsson, managing director at IMO, participated in a session on the potential effects of volcanic ash clouds from Icelandic volcanoes on aviation in the Arctic airspace. In a special session on issues related to Arctic Freshwater, Halldór Björnsson and Þorsteinn Þorsteinsson contributed to a discussion on freshwater fluxes /about-imo/news/imo-at-the-arctic-circle-assembly-2017
  • 39. The segmented dyke intrusion explained

    to time of occurrence and the colour code is shown at the top of the map. The earthquake locations delineate the track of the dyke intrusion from Bárðarbunga volcano to the eruption site at Holuhraun. Vertical cross sections through the crust are also shown; looking from the south (below) and east (to the right). Triangles mark the locations of seismic stations in and around the glacier. Data /about-imo/news/nr/3038
  • 40. Eyjafjallajökull eruption 2010 - the role of IMO

    in April-May 2010, IMO monitored the volcanic activity through various geophysical sensors (seismic, strain, GPS), river runoff from the glacier and the behaviour of the volcanic eruption cloud (see slide show). The main tool for monitoring the volcanic cloud was a C-band weather radar located at Keflavik international airport, approximately 150 km west of the volcano (see map below). Plume height /earthquakes-and-volcanism/articles/nr/2072

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