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• 31. Small glacial outburst floods around Mýrdalsjökull

  the floodwater as it emerges from the glacier. Measurements late on 9 July showed that gas levels were dangerously high at edge of Sólheimajökull, close to where floodwater is draining. We urge people not to visit the western side of Sólheimajökull where floodwater is draining from the ice. The mixture of geothermal gases in this area could cause eye irritations and breathing problems. Note /about-imo/news/nr/2917

• 32. Grímsvötn eruptions

  ) that caused global cooling and is sometimes mentioned as one of the triggers for the French revolution.Grímsvötn 21 May 2011. Photo: Ólafur Sigurjónsson.For more information on the Grímsvötn volcanic system, visit Calalogue of Icelandic volcanoes. Related topics /volcanoes/about-volcanoes/grimsvotn/

• 33. Doctoral Student Position

  /nonam/news/nr/2171

• 34. PhD Workshop 2012

  are linked to the first four theme areas of the Conference, which are listed at the Conference website as: (1) Risk assessment and impact response (2) Vulnerability and adaptive capacity (3) Building resilience, and (4) Policy development and implementation. However, an additional focus that cuts across these four themes is also pursued for the PhD Workshop, relating to: Decision making /nonam/adaption/phd-workshop-2012/

• 35. Ice cave in Hofsjökull – a warning

  and damage to the eyes. The measurements were for only one visit. It is possible that higher concentrations of gases may accumulate in the cave. It is unknown what concentration of gas the above mentioned child was exposed to.The cave should not be entered without gas monitoring instruments that can give warnings of dangerously high concentrations of H2S. We urge people to avoid such high /about-imo/news/ice-cave-in-hofsjokull-a-warning

• 36. Hekla

  changes with time during the eruption. The opening phase has the highest SiO2 content, and while the eruption is ongoing the SiO2 lowers. This explains why tephra layers from Hekla often have a light coloured base and a dark top, making ideal markers of the layers. For more information on the Hekla volcanic system, visit Catalogue of Icelandic Volcanoes /volcanoes/about-volcanoes/hekla/

• 37. Öræfajökull

  occurred 291 years ago in 1727. For more information on the Öræfajökull volcanic system, visit Catalogue of Icelandic volcanoes . .slider .level1 li li.special, .slider .level1 li li.special a { width: 40px; } North /volcanoes/about-volcanoes/oraefajokull/

• 38. Katla

  associated with Eruptions from Katla, as the magma melts the glacier while heading to the surface. For more information on the Katla volcanic system, visit the Catalogue of Icelandic VolcanoesMonitoring KatlaSeismisity GPS | GPS Monitoring Kindly study the Terms and conditions which apply to usage of data from the Icelandic Meteorological /volcanoes/katla/

• 39. Katla eruptions

  to travel west of the Mýrdalsjökull glacier but all floods after The Eldgjá event have gone down to the flood plains SE of the Mýrdalsjökull ice-cap. For more information on the Katla volcanic system, visit the Catalogue of Icelandic volcanoes.Photo: Kjartan Guðmundsson, 1918 /volcanoes/katla/katla-eruptions/

• 40. Safetravel

  telecommunication Accommodation (GPS coordinates) and other places you plan to visit/stop at Few words about the equipment Plan B Travellers can leave their travel plan with ICE-SAR, provided it includes a contact or relative whose responsibility is to alert ICE-SAR if the travellers do not arrive at the right time. ICE-SAR also provides a more extensive service with shared responsibility /about-imo/news/nr/2497