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• 11. Eyjafjallajokull_status_2010-06-11_IES_IMO

  water to flow up onto a road west of a bridge, as there it now not much difference between the height of the bridge and the river channel. Conditions at eruption site: A lake, about 300 m in diamenter, has formed at the bottom of the big crater. Steam is rising from the rims, especially from the north side. In the morning the steam cloud only rose about 100 m over the crater /media/jar/Eyjafjallajokull_status_2010-06-11_IES_IMO.pdf

• 12. norsem_ragnar

  at depth, until after the big earthquake. So the result was many “hindsight predictions” and very few successful “pre-earthquake predictions”. These mistakes are gradually convincing more and more scientists that we cannot assume that pre-earthquake activity is the same before any two earthquakes, so statistics does not work at this level. But these early precursor studies had the very /media/norsem/norsem_ragnar.pdf

• 13. Hare_2-participation

  either may not not used • OR which are simply reinforced through the participatory process – Local knowledge may not be as good as it´s made out to be – Participatory dependency As a result, mistakes can be made ● Where's my building gone? ● Your friend is a friend of the Boss? ● The need for a good view... ● What, the minister has already made a decision? How do you design long, meaningful /media/loftslag/Hare_2-participation.pdf

• 14. Safetravel in winter

  this – don't worry – you are not disturbing anyone – except for our big computer who wants to be disturbed. 112 Iceland should not be used as the only telecommunications equipment. Based on coverage and conditions it is possible that a satellite phone is needed. In many rural areas, as well as the highlands, there is no mobile coverage. Nothing can replace the safe measure of leaving a travel /about-imo/news/nr/3220

• 15. Landslides

  is usually easily eroded. If the mass is big enough, the momentum and speed can become sufficiently large to snatch up bridges, buildings or other infrastructure and therefore cause large amount of damages. One of the most infamous hazard caused by lahars occurred after the eruption in Pinatubo in 1991. https://pubs.usgs.gov/fs/1997/fs114-97/ Another example is the devastating lahar /volcanoes/volcanic-hazards/landslides/

• 16. Lava flows

  : Type of the magma and its viscosityThe steepness of the slope surface.If the magma flows as one big spread or in a narrow channel or a magma tunnel.The rate of the magma coming from the ventBasaltic magma can flow tens of kilometers from the eruption vent and the margin of the lava can go up to 10 km/hour depending on slope. Usually the transport time is shorter, but if the slope gradient /volcanoes/volcanic-hazards/lava-flow/

• 17. Bárðarbunga earthquakes 3D

  is generally considered to be the onset of this sequence of events. The size is not indicated, all the dots are equally big. Same earthquakes are shown on the topographic map as in the 3D above, for easy grasping of facts. The height is exaggerated by factor 5 in order to bring forth the landscape. The dept is also multiplied by 5 in order to distinguish between the earthquakes. Location, depth and age /earthquakes-and-volcanism/articles/nr/2948

• 18. Eyjafjallajokull_status_2010-06-07_IES_IMO

  ) observed two small flashes of lightning in the evening of 4 June. Four lightning flashes were recorded yesterday morning, 6 June. Noises: Considerable rumbling was heard at Raufarfell (10 km south of the crater) in the afternoon of 4 June. Meltwater: Low discharge from Gígjökull. Conditions at eruption site: Considerable steam emanates from the big crater and has increased since 3 /media/jar/Eyjafjallajokull_status_2010-06-07_IES_IMO.pdf

• 19. Traffc-maintenance_expenditures

  010 35 826 31 995 14 697 - - 11 565 965 240 1 534 288 1989 99 043 344 975 25 658 417 254 - 6 616 27 444 37 107 11 469 - - - 969 568 1 626 822 1988 89 553 316 711 32 055 370 248 - 4 552 24 027 41 360 9 665 - - - 888 171 1 609 435 1987 95 558 294 548 31 938 366 374 - 7 647 22 013 38 900 11 006 - - - 867 984 1 656 504 1986 70 968 273 286 26 725 324 820 - 7 254 19 103 29 614 11 425 - - - 763 193 1 521 /media/loftslag/Traffc-maintenance_expenditures.pdf

• 20. VAT_newsletter_2018_06

  Lifandi kennslu stofa í lolags breytingumA natural laboratory to study climate change Jöklar ÍslandsIcelandic glaciers Yrlit um íslenska jökla í árslok  Jöklar á Íslandi hafa hopað hratt í rúma tvo áratugi og er rýrnun þeirra einhver helsta aeiðing hlýnandi loslags hérlendis og skýr vitnis burð- ur um hlýn un ina. Hér er gerð stutt grein fyr ir breytingum á jökl un um síðan um aldamótin /media/Eplicanámskeið/VAT_newsletter_2018_06.pdf