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• 41. Articles

  descended into the caldera lake (Lake Öskjuvatn). It is one of the largest known rockslides since the settlement of Iceland. The slide covered most of the Suðurbotnahraun lava field and it reached the Kvíslahraun lava, but the eruptive fissure of the Suðurbotnahraun lava is beside the rockslide and therefore intact. The slide triggered a tsunami in the lake that washed up on the lakeshores all around /avalanches/articles/bigimg/2929

• 42. The reception at the Icelandic Met Office and projects

  the new building. Solving IMO's housing problems has been an issue for a long while. In addition to the building at Bústaðavegur 9, that was taken into use in 1973, IMO has had facilities in more than one other place in the Reykjavík area. The minister announced the plan to start preparations for a new building soon. The Icelandic Met Office gathers the most data relating to nature of all /about-imo/news/2011/nr/2412

• 43. Grímsvötn eruptions

  in the central volcano and are believed to last from a few days up to 7 months. Activity is periodic with episodes of high activity (60-80 years) with 6-11 eruptions per 40 years, alternating with low activity episodes (60-80 years) with 0-4 eruptions per 40 years. Four large effusive eruption are confirmed during the last 8000 years. The youngest one is the 1783-1784 Laki fires (Skaftáreldar in Icelandic /volcanoes/about-volcanoes/grimsvotn/

• 44. The volcano measured

  thickness is 10-12 meters and estimated volume of eruptive material 22-24 million cubic meters (only one fifth of Hekla 2000). Accordingly, the average flow rate has been approximately 15 cubic meters per second since the eruption began. The eruptive cone stands 82 m above previous ground level and the highest peak is 1067 m a.s.l. On their web-site, explanatory photographs can be found (pdf 1.1 Mb /about-imo/news/nr/1862

• 45. Ash plume and lightnings

  Ash plume and lightnings Flash flood unlikely 22.5.2011 The eruption in Grímsvötn began after 17:30 on Saturday May 21st (see photos). The altitude of the plume is monitored by two weather radars, one located /about-imo/news/nr/2177

• 46. The reception at the Icelandic Met Office and projects

  the new building. Solving IMO's housing problems has been an issue for a long while. In addition to the building at Bústaðavegur 9, that was taken into use in 1973, IMO has had facilities in more than one other place in the Reykjavík area. The minister announced the plan to start preparations for a new building soon. The Icelandic Met Office gathers the most data relating to nature of all /about-imo/news/nr/2412

• 47. Factsheet_Bardarbunga_20150303-b

  for that assignment. The Scientific Advisory Board will meet again next Tuesday, 10th of March, based on that meeting it will be decided if the hazard assessment and the restricted area will be changed. Status:  The volcanic eruption in Holuhraun came to an end on Friday 27th of February.  Seismic activity in Bárðarbunga continues to diminish. Only one earthquake stronger than M2.0 /media/jar/Factsheet_Bardarbunga_20150303-b.pdf

• 48. Sea ice in June 2008

  in Skagi. The first one on June 3rd at Þverárfjall and the latter in Hraun in Skagi on the 16th. Sea ice was not very close to shore in spite of this and the bears probably had to swim quite far. The prior bear was seen a few days after the Coast Guard went on an exploration flight on the 29th, when the ice edge came closest to shore some 35n.m. north off Kögur. Chances are that the bear /sea-ice/monthly/2008/nr/2315

• 49. 100 years since Katla erupted

  100 years since Katla erupted 12.10.2018 Today, 12 October, is the 100-year anniversary of the 1918 eruption of Katla. The volcano is considered one of the most hazardous of Iceland's 32 active volcanic systems. During the last 1100 years /about-imo/news/100-years-since-katla-erupted

• 50. A strong

  was raised to uncertainty stage. The earthquakes are of tectonic origin and located close to the junction of Húsavík-Flatey fault and Eyjafjarðaráll graben which are part of the Tjörnes Fracture Zone (TFZ). A strong earthquake swarm occurred last in this area in 2012-2013 and then four earthquakes above M5.0 were measured. An eyewitness photograph of one of the landslides that occurred in one /about-imo/news/a-strong-earthquake-swarm-offshore-north-iceland