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  • 51. 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
  • 52. 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
  • 53. 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
  • 54. Global Cryosphere Watch

    of the Implementation Meeting 22.11.2011 Director General Árni Snorrason is now in Geneva, at the first session of the GCW Implementation Meeting, held 21-24 November 2011 by the World Meteorological Organization (WMO). GCW is one of the projects of the Panel on Polar /about-imo/news/nr/2390
  • 55. norsem_slunga

    stiff machines) but also brittle stable slip. Cook studied the slip behaviour at different pressures and temperatures. He found that at shallow depths one expect in general brittle and stable slip (not unstable slip, earthquakes). This prevailed for the top 5 km of granitic crust. Between 5 and 20 km depth one got brittle unstable slip and when temperature and depth increased one got eventually /media/norsem/norsem_slunga.pdf
  • 56. Home-page - Icelandic Meteorological Office

    glacier compared to previous week with a M3.2 in Bárðarbunga caldera on April 23rd and on the same date three events of M2.5 and above were located in Grímsvötn, the largest one of M3.3. Activity in Askja and Heðurbreið was less than previous week but three earthquakes were located in Geitlandsjökull glacier. One event was located in Fljót in Skagafjörður, of M2.8, where earthquakes are rare but have /
  • 57. Weather radars

    the Icelandic Meteorological Office’s weather radars. One is located next to the airport at Keflavík and the other at Teigsbjarg in the East. On the combined images, the radar images are combined with a thermal image from the weather satellite Meteosat-9, which belongs to the European Organisation for the Exploitation of Meteorological Satellites EUMETSAT /weather/observations/radar/
  • 58. Hofsjökull ice-cap

    Hofsjökull ice-cap A new cauldron confirmed 11.10.2013 An excursion on 9 October 2013 has confirmed that a new cauldron has formed in one of Iceland's ice caps, Hofsjökull, as a result of a jökulhlaup from a subglacial, geothermal area. This image from Landsat 8 /about-imo/news/nr/2768
  • 59. Monitoring device rescued from the lava

    device rescued from the lava 13.1.2015 One of IMO's SO2 monitoring devices, which had been trapped by the Holuhraun lava flow since last year, was rescued on Saturday, 10 January. Participants of this salvaging operation were Ármann Höskuldsson, Gro Birkefeld /about-imo/news/nr/3060

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