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  • 51. Earthquakes shake Bláfjöll ski-area

    around M4 occurred, only 5 seconds apart, 6 km south of Bláfjöll mountains. Several smaller aftershocks were recorded. The earthquakes were felt widely in the capital area, and also in Ölfus and Akranes. The earthquakes are located on the tectonic plate boundary that lies eastwards along the Reykjanes peninsula where earthquakes of magnitude around M6 can occur. Largest known earthquakes /about-imo/news/earthquakes-around-blafjoll-ski-are
  • 52. Impending outburst flood in Skaftá: Likely hazards

    part of Skaftárjökull and Tungnárjökull, where floodwater could burst through the surface. Background Floods in Skaftá are sourced from two ice cauldrons, formed due to persistent geothermal activity beneath Vatnajökull ice-cap. On average, the cauldrons drain every two years, producing floods of up to 1,500 cubic metres per second. When the interval between floods is short the flood tends /about-imo/news/nr/2722
  • 53. Flood subsiding

    Skaftá river 21.1.2014 The glacial outburst flood is thought to have peaked yesterday. Floods in Skaftá are sourced from two ice cauldrons, formed due to persistent geothermal activity beneath Vatnajökull. On average, the cauldrons drain every two years, producing floods /about-imo/news/nr/2823
  • 54. A reconnaissance flight with TF-SIF

    and the river. Although it turned out to be cloudy and the visibility impaired, the radar imaging was successful. If the present seismic activity in Bárðarbunga leads to an eruption and consequently a glacial outburst flood (jökulhlaup), these images will become an important dataset for estimating the changes which may occur on the glacier and on the flooded area. Fig. 1 View to the south across /about-imo/news/nr/2953
  • 55. The FutureVolc project and the eruption on National Geographic

    Amounts of Lava, With No Signs of Slowing „A tremendous gush of lava in Iceland that began six weeks ago shows no signs of slowing. The eruption, on a plain of old lava called Holuhraun in the Bárðarbunga volcanic system, has spewed out enough molten rock so far to fill 740 Empire State buildings and has buried, on average, an area the size of an NFL football field every 5.5 minutes /about-imo/news/nr/3003
  • 56. The earthquake swarm on Reykjanes ridge

    eruptive activity with two recognized eruptions per century. IMO is currently using the Aviation Color Code to report the status of active volcanic systems in Iceland and provide warning related to unusual activity. Based on the evidence that the current seismicity is well above the normal (monthly averaged) background condition, IMO's scientists decided to raise the aviation color code, AVCC /about-imo/news/nr/3163
  • 57. Glacial outburst flood probably in progress

    in Vatnajökull is also being closely monitored (see plot 17 - 29 September), the last jökulhlaup from there having occurred in 2010. Remark 29.9.2015 at 22:28: Floodwater is beginning to drain from the eastern Skaftá ice-cauldron, located beneath Vatnajökull. According to GPS measurements, the ice-surface above the lake began to subside late on 27 September. The rate of subsidence is increasing /about-imo/news/nr/3199
  • 58. Prohibited area around the Holuhraun lava field

    and to the westernmost branches of Jökulsá á Fjöllum in the west. Enlarge. Preliminary flood risk assessment Preliminary flood risk assessment for Jökulsá á Fjöllum gives flood travel times in minutes. The assigned locations (dots) are colour coded: Red location (dot) is half an hour from the source, orange is an hour, dark yellow one and a half hours, bright yellow two hours, light green two and a half /hydrology/articles/nr/2963
  • 59. Lightning

    Lightning is an electric current through air that occurrs when charge difference between two points in the air is quite high. The electric current causes a powerful electromagnetic wave in all directions. Thunderstorms are not common in Iceland comparted to more southerly countries. Information on measured lightning in Iceland for the past days can be found on IMO's webpage. Lightning can /volcanoes/volcanic-hazards/lightnings/
  • 60. Earthquake activity east of Grímsey has decreased

    April (18:30). The activity continued with gradually decreasing intensity the following day on both clusters. Around midnight, however, two earthquakes of magnitude 3.4 and 3.6 occurred in the northwestern part of the cluster and were felt in Grímsey. This led to a temporary increase in activity, which since then has been slowly decreasing. Below is a map of the bathymetry east of Grímsey /about-imo/news/nr/2685

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