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• 21. 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

• 22. 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/

• 23. VI2010-006_web

  og hart sem skýra má með því að það hafi verið undir þungu fargi jökulíss. Akureyrarbrekkurnar eru í aðalatriðum bakkar sem myndaðir eru í þessi þéttu setlög, allt að 60 m háir, en nyrsti hluti brekknanna eru há klappar- holt. Yfirborð er nú gróið og þakið jarðvegi en ýmislegt bendir þó til þess að fyrir 200–300 árum hafi brekkurnar verið mikið til gróðurvana. Áður gekk sjór víðast alveg að /media/vedurstofan/utgafa/skyrslur/2010/VI2010-006_web.pdf

• 24. A minor eruption underway

  imagery. The eruption site is in a valley, about 4.7 km inland from the southern coast of the peninsula. The coastal town of Grindavík is the closest populated region to the eruption site, located approximately 10 km to the southwest.The eruption is considered small at this stage and the eruptive fissure is appr. 200 m long. The area of the lava is covering an area that is appr. 500 m wide /about-imo/news/earthquake-swarm-in-reykjanes-peninsula

• 25. Pollution

  Vestmannaeyjar, 12 km off the south coast of Iceland. It is surrounded by sea to the east, south and west. The elevation above sea level is 118 m. Distance from the fishing town on the island is 4.5 km, distance to the nearest village on shore is 40 km and distance to the nearest town on shore is 70 km. That town has less than 5000 inhabitants. This is an ideal seashore background station at 63°N, 20°W /pollution-and-radiation/pollution/

• 26. Flood in Grímsvötn

  is calculated to be around 5000 m3/s. This size of flood will most likley not affect the infastructure in the area such as roads or bridges. These forecasts are uncertain at this early stage. There are past examples of Grímsvötn eruptions starting following a flood. The loss of the water from Grímsvötn lake reduces the pressure on top of the volcano and this can allow an eruption to begin /about-imo/news/icesheet-in-grimsvotn-subsiding

• 27. Group3-Road-scenarios

  in five-year basis  Current state of the road network affects the possible decisions to be made at the moment Political adaptation Management structures have to be more flexible and ready to apply adaptive management Technological adaptation 0 1000 2000 3000 4000 5000 6000 1985199019952000200520102015202020252030 vans (mln. tonkm) lorries (mln. tonkm) 0 10000 20000 30000 /media/loftslag/Group3-Road-scenarios.pdf

• 28. Refsgaard_2-uncertainty

  /breakthrough curves West East Model C Model A Model B Fractured clay/ Toplayer Sand Clayey till Limestone SelandienLimestone 0 20 40 60 0 0.2 0.4 0.6 0.8 1 N or m al is ed c on ce nt ra ti on 0 20 40 60 80 100 0 0.2 0.4 0.6 0.8 1 0 40 80 120 160 200 Time in years 0 0.2 0.4 0.6 0.8 1 N or m al is ed c on ce nt ra ti on 0 100 200 300 Time in years 0 0.2 0.4 0.6 0.8 1 Model A Model B Model C Simulated /media/loftslag/Refsgaard_2-uncertainty.pdf

• 29. askja_minnisblad_ens

  Minnisblað ___________________________________________________ 7 Figure 8. Right: An areal photo of the rockslide area in Suðurbotnar. There is evidence of older movement which is probably an old rockslide. Left: The outline of the rockslide. The lake shore has retreated in places (yellow areas), the displacement being up to 50 m. Around the middle of the deposit /media/ofanflod/myndasafn/frodleikur/askja_minnisblad_ens.pdf

• 30. Rockslide in Askja, July 21 2014 - Preliminary results of observations

  : The outline of the rockslide. The lake shore has retreated in places (yellow areas), the displacement being up to 50 m. Around the middle of the deposit, the edge seems to have advanced (purple area). Background: Loftmyndir ehf. Analyses: Ásta Rut Hjartardóttir and Þorsteinn Sæmundsson. Fig. 9 Figure 9. Geological map showing the outline of the rockslide, as well as eruptive fissures /avalanches/articles/nr/2929