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  • 51. Factsheet_Bardarbunga_20150203

    continues until the subsidence of the Bardarbunga caldera stops. The eruption can still go on for many months.  The volcanic fissure may lengthen southwards under Dyngjujokull, resulting in a jokulhlaup and an ash- producing eruption. It is also possible that eruptive fissures could develop in another location under the glacier. If such an eruption would be prolonged it could eventually /media/jar/Factsheet_Bardarbunga_20150203.pdf
  • 52. Factsheet_Bardarbunga_20150206

    of the cloud) and how they were affected by it. • The volcanic eruption has now been going on for five months, the lava flow is still great in Holuhraun and the rate of the subsidence of the Bardarbunga caldera is still significant. Three scenarios are considered most likely: • The eruption in Holuhraun continues until the subsidence of the Bardarbunga caldera stops. The eruption can still go /media/jar/Factsheet_Bardarbunga_20150206.pdf
  • 53. Factsheet_Bardarbunga_20150210

    until the subsidence of the Bardarbunga caldera stops. The eruption can still go on for many months. • The volcanic fissure may lengthen southwards under Dyngjujokull, resulting in a jokulhlaup and an ash- producing eruption. It is also possible that eruptive fissures could develop in another location under the glacier. If such an eruption would be prolonged it could eventually produce a lava /media/jar/Factsheet_Bardarbunga_20150210.pdf
  • 54. Factsheet_Bardarbunga_20150213

    significant. Three scenarios are considered most likely:  The eruption in Holuhraun continues until the subsidence of the Bárðarbunga caldera stops. The eruption can still go on for many months.  The volcanic fissure may lengthen southwards under Dyngjujökull, resulting in a jökulhlaup and an ash- producing eruption. It is also possible that eruptive fissures could develop in another /media/jar/Factsheet_Bardarbunga_20150213.pdf
  • 55. Factsheet_Bardarbunga_20150217

    by it.  The volcanic eruption has now been going on for over five months, the lava flow is still great in Holuhraun and the rate of the subsidence of the Bárðarbunga caldera is still significant. Three scenarios are considered most likely:  The eruption in Holuhraun continues until the subsidence of the Bárðarbunga caldera stops. The eruption can still go on for many months /media/jar/Factsheet_Bardarbunga_20150217.pdf
  • 56. Factsheet_Bardarbunga_20150220

    flow has decreased substantially in Holuhraun and the rate of the subsidence of the Bárðarbunga caldera has also decreased substantially. Three scenarios are considered most likely:  The eruption in Holuhraun continues until the subsidence of the Bárðarbunga caldera stops. The eruption could come to an end in the next few weeks but it cannot be ruled out that a small eruption could go /media/jar/Factsheet_Bardarbunga_20150220.pdf
  • 57. Factsheet_Bardarbunga_20150224

    :  The eruption in Holuhraun continues until the subsidence of the Bárðarbunga caldera stops. The eruption could come to an end in the next few weeks but it cannot be ruled out that a small eruption could go on for many months.  The volcanic fissure may lengthen southwards under Dyngjujökull, resulting in a jökulhlaup and an ash- producing eruption. It is also possible that eruptive fissures could /media/jar/Factsheet_Bardarbunga_20150224.pdf
  • 58. Factsheet_Bardarbunga_20150227

    caldera stops. The eruption could come to an end in the next few weeks but it cannot be ruled out that a small eruption could go on for many months.  The volcanic fissure may lengthen southwards under Dyngjujökull, resulting in a jökulhlaup and an ash- producing eruption. It is also possible that eruptive fissures could develop in another location under the glacier. If such an eruption would /media/jar/Factsheet_Bardarbunga_20150227.pdf
  • 59. bb100days_ens

    Gas measurements The ongoing eruption at Holuhraun is very rich in gas. We should go 150 years back to find an event (Trolladyngja) that had a comparable impact on Iceland and its inhabitants, in terms of enviromental and health issues. IMO is monitoring gas releases from Holuhraun using DOAS and FTIR instruments for the estimation of SO2 flux and amount of other components /media/jar/bb100days_ens.pdf
  • 60. Factsheet_Bardarbunga_140914

    breaking out from the main lava stream towards the east and west. The largest one of these lava tongues stretches towards the east and had become 300 m wide and 2 km long at 18:00 yesterday. An eruption cloud reaches 4 km in height but lowers with distance from the eruption site.  Seismic activity is similar to what it has been in the past days but earthquakes are starting to go down in numbers /media/jar/myndsafn/Factsheet_Bardarbunga_140914.pdf

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