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• 21. VI_2013_006

  <6h <12h <24h Total Grímsvötn 1998-12-18 09:20 2 h 0 1 20 121 167 183 Hekla 2000-02-26 18:17 41 min 1 4 6 6 6 6 Grímsvötn 2004-11-01 21:50 4 h 0 0 15 59 142 251 Fimmvörðuháls 2010-03-20 23:34 - 0 0 0 0 0 0 Eyjafjallajökull 2010-04-14 01:15 17 h 0 0 0 0 10 790 Grímsvötn 2011-05-21 19:00 15 min 888 3340 6484 11729 16041 16195 9 The monitoring system There are two main parts /media/vedurstofan/utgafa/skyrslur/2013/VI_2013_006.pdf

• 22. 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/

• 23. Risk Assessments

  riskianalyysit - ilmaston muutoksen synnyttämät riskit ja mahdollisuudet. 12.03.2009, Research Report VTT-R-01942-09, Tampere. 13 p. + app. 24 p. Linnerud, Kristin (2009) Test and evaluation of a climate risk assessment procedure. Case study: The Norwegian hydro power company SFE. CICERO, University of Oslo. Report 2009:3. Feb.2009. 44 p. ISSN:0804-4562. Linnerud, Kristin (2009) Climate change /ces/publications/nr/1941

• 24. CASE_B__Heikki_Tuomenvirta_(FMI)_Introduction

  of climate change on the routine and periodic maintenance of roads. Helsinki 2009. Finnish Road Administration, Central Administration. Finnra reports 8/2009, 66 p. + app. 8 p. ISSN 1459-1553, ISBN 978-952-221-172-9, TIEH 3201122-v. (in Finnish, abstract in English) [5] Salanne, i., Byring, B., Valli, R., Tikkanen, R., Peltonen, P., Haapala, J., Jylhä, K., Tolonen-Kivimäki, O., and Tuomenvirta, H /media/loftslag/CASE_B__Heikki_Tuomenvirta_(FMI)_Introduction.pdf

• 25. 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

• 26. 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/

• 27. VI_2020_011_en

  An initial volcanic hazard assessment of the Vestmannaeyjar Volcanic System: Impacts of lava flow and tephra deposit on Heimaey Melissa Anne Pfeffer, Sara Barsotti, Esther Hlíðar Jensen, Emmanuel Pierre Pagneux, Bogi Brynjar Björnsson, Guðrún Jóhannesdóttir, Ármann Höskuldsson, Laura Sandri, Jacopo Selva, Simone Tarquini, Mattia de´Michieli Vitturi, Ingibjörg Jónsdóttir, Davið Egilson /media/vedurstofan-utgafa-2020/VI_2020_011_en.pdf

• 28. 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

• 29. 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

• 30. VED_AnnualReport-2013_screen

  as river discharge and water levels. Notices on avalanches and sea-ice are shown; short articles and news are presented. Furthermore, web and data portals can be accessed through the web, which is available in both Icelandic and English. IMO uses the social networking website Facebook for communication and feed-back. A new web-application (App) provides access to forecasts and warnings /media/vedurstofan/utgafa/arsskyrslur/VED_AnnualReport-2013_screen.pdf