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• 11. Öræfajökull – frequent questions & answers

  to melt. The pyroclastic flows and jökulhlaup caused by the 1362 eruption are thought to have resulted in the death of ~300 individuals. The magnitude of the 1362 jökulhlaup was of order 100,000 m3/s, whereas the 1727 flood was about half that size. In 1362 tephra fallout buried houses and villages with a deposit >40cm thick.The Öræfajökull eruption in 1362 has been one of the largest eruption /volcanoes/about-volcanoes/oraefajokull/q-a/

• 12. Iceland a member of ECMWF

  day of the second month following the deposit of its instrument of accession. Svandís Svavarsdóttir: “It is an honour for me to sign the accession agreement with the European Centre for Medium-Range Weather Forecasts, one of the world’s leading centres in numerical weather prediction. This is a major milestone for Iceland in establishing closer links to European centres of excellence /about-imo/news/nr/2142

• 13. Iceland a member of ECMWF

  day of the second month following the deposit of its instrument of accession. Svandís Svavarsdóttir: “It is an honour for me to sign the accession agreement with the European Centre for Medium-Range Weather Forecasts, one of the world’s leading centres in numerical weather prediction. This is a major milestone for Iceland in establishing closer links to European centres of excellence /about-imo/news/2011/nr/2142

• 14. Iceland a member of ECMWF

  day of the second month following the deposit of its instrument of accession. Svandís Svavarsdóttir: “It is an honour for me to sign the accession agreement with the European Centre for Medium-Range Weather Forecasts, one of the world’s leading centres in numerical weather prediction. This is a major milestone for Iceland in establishing closer links to European centres of excellence /about-imo/news/nr/2142/

• 15. Iceland a member of ECMWF

  day of the second month following the deposit of its instrument of accession. Svandís Svavarsdóttir: “It is an honour for me to sign the accession agreement with the European Centre for Medium-Range Weather Forecasts, one of the world’s leading centres in numerical weather prediction. This is a major milestone for Iceland in establishing closer links to European centres of excellence /about-imo/news/2011/nr/2142/

• 16. FAQ

  meters-size (bombs and ballistics) can land up to few km from the vent and can represent a serious hazard in the proximity of a volcano. Those particles that decouple quickly from the volcanic plume due to their size and weight fall close to the volcano and constitute the proximal deposit. Smaller particles can reach higher altitudes and persist in the atmosphere for days and weeks /volcanoes/grimsvotn-activity/faq/

• 17. Traffc-maintenance_expenditures

  1965 7 549 30 414 3 555 86 331 - 813 - 1 065 - - - - 129 728 1 823 901 1964 5 392 27 038 1 611 70 991 - 1 090 - 2 043 - - - - 108 166 1 603 671 1963 4 275 24 368 1 682 54 879 - 462 - 2 492 - - - - 88 158 1 382 441 1962 3 632 22 117 2 313 52 079 - 168 - 3 633 - - - - 83 941 1 396 905 1961 3 249 18 138 2 313 52 276 - 118 - 3 934 - - - - 80 028 1 388 467 1960 2 800 16 168 1 514 53 793 - 128 - 3 491 /media/loftslag/Traffc-maintenance_expenditures.pdf

• 18. VI_2009_006_tt

  during the Holocene . . . . . . . . . . . . . . 6 2.5 Jökulhlaups in America and Asia at the end of the last glaciation . . . 7 2.6 Jökulhlaup sediment concentration and Lahars . . . . . . . . . . . . . 8 3 The Skaftá cauldrons and jökulhlaups in Skaftá 9 3.1 The subglacial lakes . . . . . . . . . . . . . . . . . . . . . . . . . . . 9 3.2 Jökulhlaups in Skaftá /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_006_tt.pdf

• 19. A large landslide falls in Hítardalur valley

  displacements and might be an old landslide deposit. The displaced material is a mixture of e.g. rock debris, scree from the lower part of the hillside, swamp soil and sediments from ancient lakes on the valley bottom. A preliminary estimate of the volume of the slide is 10–20 million m3. The area of the debris tongue is ca. 1,5 km2 and the debris is up to 20–30 m thick. The thickness is 5–10 m in many /about-imo/news/a-large-landslide-falls-in-hitardalur-valley

• 20. A large landslide falls in Hítardalur valley

  displacements and might be an old landslide deposit. The displaced material is a mixture of e.g. rock debris, scree from the lower part of the hillside, swamp soil and sediments from ancient lakes on the valley bottom. A preliminary estimate of the volume of the slide is 10–20 million m3. The area of the debris tongue is ca. 1,5 km2 and the debris is up to 20–30 m thick. The thickness is 5–10 m in many /about-imo/news/a-large-landslide-falls-in-hitardalur-valley/