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  • 51. Supporting structures stopped most of an avalanche

    structures are shown as black dashed lines. It may be estimated that 5,000-10,000 m³ of snow were stopped in the rows of supporting structures. This is many times the volume of snow in the avalanche tongue below the structures. The snow cover above the topmost row did not move or break up. It is possible that this is due to the supporting structures but as the fracture line to the west /about-imo/news/nr/2476
  • 52. Supporting structures stopped most of an avalanche

    of supporting structures are shown as black dashed lines. It may be estimated that 5,000-10,000 m³ of snow were stopped in the rows of supporting structures. This is many times the volume of snow in the avalanche tongue below the structures. The snow cover above the topmost row did not move or break up. It is possible that this is due to the supporting structures but as the fracture line /avalanches/articles/nr/2475
  • 53. Photos from Eyjafjallajökull

    Articles Black eruption plume above low clouds /earthquakes-and-volcanism/articles/nr/1904
  • 54. Supporting structures stopped most of an avalanche

    ). The narrow curves show outlines of historical avalances. The health care centre is the large H-shaped building close to the hillside. The rows of supporting structures are shown as black dashed lines. It may be estimated that 5,000-10,000 m³ of snow were stopped in the rows of supporting structures. This is many times the volume of snow in the avalanche tongue below the structures. The snow cover /about-imo/news/nr/2476/
  • 55. Supporting structures stopped most of an avalanche

    red curve). The narrow curves show outlines of historical avalances. The health care centre is the large H-shaped building close to the hillside. The rows of supporting structures are shown as black dashed lines. It may be estimated that 5,000-10,000 m³ of snow were stopped in the rows of supporting structures. This is many times the volume of snow in the avalanche tongue below the structures /avalanches/articles/nr/2475/
  • 56. Grimsvotn_status_2011-05-22_IES_IMO

    of the eruption site at 14:54 hrs. Colour: Brown- or grayish and sometimes black close to the eruption site. Tephra fallout: The amount of fallout is massive east from Kirkjubæjarklaustur west to the center of Mýrdalssandur. The visibility is virtually zero. The fallout is most concentrated south of the volcano, but less dense to the north and east. Lightning: This afternoon, lightning /media/jar/Grimsvotn_status_2011-05-22_IES_IMO.pdf
  • 57. Grimsvotn_status_2011-05-23_IES_IMO

    At altitudes of 8 km and higher, part of the plume heads to the west. Colour: Brown- or grayish and sometimes black close to the eruption site. Tephra fallout: The amount of fallout is great from Vík in the west to the east of Öræfajökull. The amount of ash fall is the greatest close to the village Kirkjubæjarklaustur. Ash has been detected in several areas throughout the country, except /media/jar/Grimsvotn_status_2011-05-23_IES_IMO.pdf

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