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• 31. On the Bárðarbunga gradual caldera collapse

  was 110 km². The large scale subsidence of calderas is considered to accompany most very large eruptions as the roof overlying a reservoir of magma in the crust under the volcano collapses and falls into it. Eruptions of this type are not common. Before Bárðarbunga, worldwide only six cases are known since the beginning of the 20th century. Moreover, the caldera collapse of Bárðarbunga is the first /about-imo/news/on-the-bardarbunga-gradual-caldera-collapse/

• 32. Öræfajökull – frequent questions & answers

  in Iceland and the second largest in Europe after the Vesuvius 79 AD. Question: What are the possible hazards related to an eruption in Öræfajökull?Answer: Tephrafallout, ash cloud, lightning, pyroclastic flows, jökulhlaup /glacial outburst floods, ballistics, lava flows, gas pollution. They will occur over different time frames, with probably the flood to be the first sub-aerial evidence /volcanoes/about-volcanoes/oraefajokull/q-a/

• 33. Workshop on Earthquakes in North Iceland

  will attend the workshop as well as representatives of the civil protection authorities and other parties who work on responding to earthquake hazard in general. The workshop has presentations related to the geological history of the area, current tectonics, earthquake activity, monitoring, on likely scenarios in case of a major event in North Iceland, and on possible precautionary measures to reduce /about-imo/news/nr/2701

• 34. Glacier mapping – IPY

  km², since some ice-free areas outside the ice caps are included, and also some areas have been measured twice for research and quality assurance purposes. Comparable digital elevation models of glaciers in Iceland have hitherto not been available. The new models will serve as a baseline for comparison with all other measurement, past and future. With repeated measurements it is possible /about-imo/arctic/glacier-mapping-ipy/

• 35. ICEWIND

  the Risø DTU National Laboratory for Sustainable Energy, the Norwegian Meteorological Institute, the University of Gotland, Statoil and the Technical Research Centre of Finland (VTT) along with many of the Nordic countries major wind energy companies. The ICEWIND's main goal is to share knowledge between the Nordic countries and identify factors that delay or prevent the adopton of wind energy /about-imo/arctic/icewind/

• 36. Map of the glaciers of Iceland

  at the peak of the so called Little Ice Age during the 1890s and also the outlines as they were around the year 2000. The map distinguishes surging glaciers from other outlet glaciers, and identifies all known sub-glacial volcanic calderas. Featured are the names of all named glaciers and the map includes a brochure and a list of glacier names. The Map of Glaciers can be used for both tourism /about-imo/arctic/map-of-glaciers/

• 37. SVALI

  The western cauldron in Vatnajökull ice cap on 19 August 2000, shortly after jökulhlaup in river Skaftá which originated in the cauldron. Photo: Oddur Sigurðsson. The SVALI project examines the complex effects of climate change on the Arctic environment, especially as glaciers, ice and snow. The projects main research questions are as follows: How fast is land ice volume in the Arctic /about-imo/arctic/svali/

• 38. Eruption on Fimmvörðuháls

  of the Eyjafjallajökull ice cap. Seismic activity in Eyjafjallajökull has been intensive for the past three weeks and most of the earthquakes have been located between 7 and 10 km depth. On March 19th a seismic swarm began east of the top crater, originating between 4 and 7 km depth. The activity migrated eastwards and towards the surface on Saturday, March 20th. At 22:30 GMT a slightly increased /about-imo/news/nr/1845

• 39. Glacier mapping – IPY

  km², since some ice-free areas outside the ice caps are included, and also some areas have been measured twice for research and quality assurance purposes. Comparable digital elevation models of glaciers in Iceland have hitherto not been available. The new models will serve as a baseline for comparison with all other measurement, past and future. With repeated measurements it is possible /about-imo/arctic/glacier-mapping-IPY/

• 40. Lidar 2013

  measurements are in widespread use for mapping changes of ice sheets and glaciers. With developments in unmanned aerial vehicles (UAVs) and terrestrial lidar, and novel photon counting techniques for both airborne and satellite applications, lidar measurements will continue to be a key tool for ice sheet and glacier monitoring, and measurement of sea ice properties. The 2-day workshop is aimed to bring /lidar/lidar-2013