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• 41. Factsheet_Bardarbunga_20141216

  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 flow.  Volcanic eruption /media/jar/Factsheet_Bardarbunga_20141216.pdf

• 42. Factsheet_Bardarbunga_20141219

  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 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 /media/jar/Factsheet_Bardarbunga_20141219.pdf

• 43. Factsheet_Bardarbunga_20141222

  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 on for many months.  The volcanic fissure may lengthen southwards under Dyngjujokull, resulting in a jokulhlaup and an ash- producing eruption /media/jar/Factsheet_Bardarbunga_20141222.pdf

• 44. Factsheet_Bardarbunga_20141230

  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 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 /media/jar/Factsheet_Bardarbunga_20141230.pdf

• 45. Factsheet_Bardarbunga_20150106

  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 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 /media/jar/Factsheet_Bardarbunga_20150106.pdf

• 46. Factsheet_Bardarbunga_20150109

  affected by it.  The volcanic eruption has now been going on for over three 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 on for many months /media/jar/Factsheet_Bardarbunga_20150109.pdf

• 47. Factsheet_Bardarbunga_20150113

  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 flow.  Volcanic eruption in the Bardarbunga caldera. Such an eruption would /media/jar/Factsheet_Bardarbunga_20150113.pdf

• 48. Factsheet_Bardarbunga_20150116

  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 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 /media/jar/Factsheet_Bardarbunga_20150116.pdf

• 49. Factsheet_Bardarbunga_20150120

  are considered most likely: • The eruption in Holuhraun 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 /media/jar/Factsheet_Bardarbunga_20150120.pdf

• 50. Factsheet_Bardarbunga_20150123

  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 flow.  Volcanic eruption in the Bardarbunga caldera /media/jar/Factsheet_Bardarbunga_20150123.pdf