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• 41. Further information regarding gas pollution

  rather than towards you.In calm/light wind (<5 m/s) gas can accumulate in the valleys, then circulation is controlled by the landscape and gas can exceed danger levels far up the slopes, all around the eruption site. In such cases, spectators need to move up to higher ground levels such as mountains and ridges and not stay on the slopes just above the eruption. Choose a walking route according /volcanoes/fagradalsfjall-eruption/volcanic-gases/

• 42. Eyjafjallajokull_status_2010-05-08_IES_IMO

  the lava edge. A small lava tunnel was observed with an infrared camera near to the crater. Seismic tremor: Low, similar to yesterday and similar amplitude on all frequency bands. Earthquakes: Less earthquake activity, two events, Ml 1.2, detected at 9 and 12 km depth at around 11:00h and two of similar magnitude around 14:00. GPS deformation: No significant changes were observed /media/jar/Eyjafjallajokull_status_2010-05-08_IES_IMO.pdf

• 43. Factsheet_Bardarbunga-140911

  o Large-scale subsidence of the caldera occurs, causing an eruption at the edge of the caldera. Such an eruption would melt large quantities of ice, leading to a major jökulhlaup. Other scenarios cannot be excluded. From the Icelandic Met Office: The Aviation Colour Code for Bárðarbunga remains at ‘orange’ but the code for Askja has been changed to ‘green’. /media/jar/Factsheet_Bardarbunga-140911.pdf

• 44. Factsheet_Bardarbunga-140912

  develop in another location under the glacier. o Large-scale subsidence of the caldera occurs, causing an eruption at the edge of the caldera. Such an eruption would melt large quantities of ice, leading to a major jökulhlaup, accompanied by ashfall. Other scenarios cannot be excluded. From the Icelandic Met Office: The Aviation Colour Code for Bárðarbunga remains at ‘orange’ and the code /media/jar/Factsheet_Bardarbunga-140912.pdf

• 45. Factsheet-Bardarbunga-20140913

  of the caldera occurs, causing an eruption at the edge of the caldera. Such an eruption would melt large quantities of ice, leading to a major jökulhlaup, accompanied by ashfall. Other scenarios cannot be excluded. From the Icelandic Met Office: The Aviation Colour Code for Bárðarbunga remains at ‘orange’. /media/jar/myndsafn/Factsheet-Bardarbunga-20140913.pdf

• 46. Latest news on the eruption at Reykjanes peninsula

  the area and to follow instructions and advice as given by the local Police and Civil Protection authorities.Updated 8.8. at 13:00Gas pollution at the eruption site can at any time exceed danger levels. The eruptive plume follows the wind direction, and it is therefore safer to watch the eruption with the wind direction behind you, rather than towards you.In calm/light wind (<5 m/s) gas can /about-imo/news/a-new-eruption-has-started-at-fagradalsfjall

• 47. Eyjafjallajökull eruption

  the eruption site have coalesced to form a larger cauldron. In spite of magma splatters, no lava flow has been detected yet. Heavy sound blasts have been heard and found near Eyjafjallajökull, especially south and east of the mountain. The viscosity of the magma from Eyjafjallajökull is higher than on Fimmvörðuháls and this enhances the explosive sound effect which can be heard over long distances /about-imo/news/nr/1887

• 48. Factsheet_Bardarbunga_20150228

  site.  No changes have been made to the restricted area north of Vatnajökull.  The Civil Protection still operates in alert phase.  Aviation Colour Code for Bárðarbunga has been downgraded from orange to yellow.  From the Icelandic Met Office: The Aviation Colour Code for Bárðarbunga has been downgraded from orange to yellow. The Aviation Colour Code system for Icelandic Volcanic /media/jar/Factsheet_Bardarbunga_20150228.pdf

• 49. News

  2010, as seen at 12:00 GMT at an elevation of 3-3.6 km (10-12,000 ft). Light coloured, low-lying clouds of steam were observed over the eruption site, together with occasional bursts of grey to black-coloured cloud, which rise to up to half of the total height of the eruption plume. Above this level, the plume was lighter in colour with a capping of white cloud (not visible here /about-imo/news/bigimg/1891

• 50. Icelandic volcanoes

  of a volcanic system is basically an attempt of geologists to simplify what is involved. Volcanic system consists of a central volcano and/or fissure swarms which extend out from a volcano. As a general rule, volcanic system is named after the central volcano. Click on the tabs on the left and you will find information on Iceland's primary volcanoes; general information about the volcano, recent /volcanoes/about-volcanoes/