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• 11. 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

• 12. 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/

• 13. 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/

• 14. 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

• 15. 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

• 16. bb100days_ens

  magnitude of 6.6 if the same energy was released in one big earthquake. This number might sound small, however it has to be kept in mind that the magnitude scale of earthquakes is logarithmic. An increase of one magnitude corresponds to an energy increase by a factor of around 30, i.e. a magnitude 5 earthquake releases around 30 times more energy than a magnitude 4. It is however worth to notice /media/jar/bb100days_ens.pdf

• 17. Factsheet_Bardarbunga_20140920

  University of Iceland along with representatives from the Icelandic Civil Protection and the Environmental Agency of Iceland. Main points  Volcanic eruption in Holuhraun  Air quality  Scenarios Notes  The volcanic eruption in Holuhraun continues with similar rate as last few days.  The subsidence of the Bardarbunga caldera continues with same rate as before.  Big earthquakes /media/jar/Factsheet_Bardarbunga_20140920.pdf

• 18. Factsheet_Bardarbunga_20140921

  as before.  Big earthquakes are still detected in the Bardarbunga caldera. Since noon yesterday there have been 18 earthquakes bigger the M3,0. The biggest one was measured M5,0 at 17:11 yesterday afternoon. Smaller earthquakes were detected in north part of the dyke and around the eruption site.  No change was detected in water monitoring that cannot be explained with changing weather /media/jar/Factsheet_Bardarbunga_20140921.pdf

• 19. Factsheet_Bardarbunga_20140922

  The lava flow is now around the centre of the lava field, which is now around 37 square kilometres. According to new measurements the total volume of the lava is 0,4-0,6 cubic kilometres and the magma flow 250-350 cubic meters pr. second.  The subsidence of the Bardarbunga caldera continues with same rate as before.  Big earthquakes are still detected in the Bardarbunga caldera. Since noon /media/jar/myndsafn/Factsheet_Bardarbunga_20140922.pdf

• 20. Group3-The-future-of-the-Finnish-national-road-network

  to the big roads (noise reduction vs. durability of asphalt), scientists in road technology, firms 0 10000 20000 30000 40000 50000 60000 1 9 8 5 1 9 9 0 1 9 9 5 2 0 0 0 2 0 0 5 2 0 1 0 2 0 1 5 2 0 2 0 2 0 2 5 2 0 3 0 pass_cars (mln. Pkm) pass_cars (mln. Pkm) Projection of passenger kilometers Socio-economic scenario Climate scenario Worst case (4.4 C increase; 17 % increase in prec /media/loftslag/Group3-The-future-of-the-Finnish-national-road-network.pdf