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• 31. field_report_04032015

  Field report - Holuhraun 4 March 2015 By Baldur Bergsson, Benedikt Ófeigsson, Richard Yeo, Sara Barsotti General description of the eruption site No signs of activity have been revealed. A diffuse bluish haze, at ground level, was visible across the lava field. The crater rim has several cracks at the very edge. While standing close to the crater rim it was possible to hear rumbling due /media/jar/field_report_04032015.pdf

• 32. Sea ice in June 2010

  an ice strip at 66°42'N and 24°15' W up to 66°59'N and 22°24'W. On the 14th an observation was also received from the weather station „Hraun á Skaga“ on an iceberg 10-11 nm northwest of Skagatá. On the 22nd an ice strip was observed at 66°49'N and 22°22'W until 66°51'N and 22°09'W. On the 29th two icebergs were observed in Þverál. IMO issued information and an image of the ice edge 16th June. Wind /sea-ice/monthly/2010/nr/2341

• 33. Bardarbunga_Daily_status_report_260814

  ) shows 90 uS/cm. Conditions at eruption site No eruption. Seismic tremor No harmonic (volcanic) tremor observed. Earthquakes Intense seismicity continues. Seismicity continues to migrate northward. Seismicity is now concentrated on the portion of the dike by the edge of the Dyngjujökull glacier. Most of the dyke-related events are at 8-12 km depth. A magnitude 4.6 earthquake, the largest detected /media/jar/Bardarbunga_Daily_status_report_260814.pdf

• 34. Eyjafjallajokull_status_2010-05-08_IES_IMO

  the rim of the ice edge around the crater. The plume does'nt rise vertically from the crater, but bends SE-wards due to wind. Plume reaches higher after larger explosions. Thephra fallout near the crater is considerably less than was observed on May 6th. There is little lava flow down Gígjökull and the lava front has not changed for the last couple of days. Very little steam rises from /media/jar/Eyjafjallajokull_status_2010-05-08_IES_IMO.pdf

• 35. Factsheet-Bardarbunga-140906

  to the recent high seismic activity and subsurface magma flow to the northeast.  In the surveillance flight yesterday a shallow, wide depression was observed on the surface of Dyngujökull, 10 km from the glacier edge. Another depression 6 km from the Dyngjujökull ice edge, which has been monitored over the last few days has deepened and is now 35 m deep. o It is likely that these depressions /media/jar/Factsheet-Bardarbunga-140906.pdf

• 36. Impending outburst flood in Skaftá: Likely hazards

  the floodwater as it drained from the Vatnajökull ice-cap. The gas is particularly potent at the ice margin, where concentrations will reach poisonous levels. If flood occurs, travellers must stay away from the edge of Skaftárjökull, Tungnaárjökull and Síðujökull. Crevasses will develop rapidly around the ice cauldron, so travellers on Vatnajökull should stay away from the region, including the lower /about-imo/news/nr/2722

• 37. Small glacial outburst floods around Mýrdalsjökull

  the floodwater as it emerges from the glacier. Measurements late on 9 July showed that gas levels were dangerously high at edge of Sólheimajökull, close to where floodwater is draining. We urge people not to visit the western side of Sólheimajökull where floodwater is draining from the ice. The mixture of geothermal gases in this area could cause eye irritations and breathing problems. Note /about-imo/news/nr/2917

• 38. A minor jökulhlaup in river Gígjukvísl

  and even damage to eyesight. For travellers on Skeiðarársandur, the ongoing flood poses no hazards. Elevated levels of seismic tremor have been recorded at IMO's seismic station on the edge of Grímsvötn. This signal is a measure of the amount of water draining from the lake. IMO continues to monitor the flood and any significant updates will be reported on the front page for hydrology. The graphs /about-imo/news/nr/3135

• 39. Prohibited area around the Holuhraun lava field

  A reduction in the access controlled area was announced 16.03.2015 (pdf 0.8 Mb). An estimate of the danger of flooding was made, see bottom of page. The restricted area extends 20 m outside the edges of the new lava field, to the edge of Dyngjujökull glacier on the south side, the river Jökulsá á Fjöllum to the east /hydrology/articles/nr/2963

• 40. IMO's glaciologist in 'NBC Today'

  from Mýrdalsjökull ice cap. In total, glacial ice covers about 11% of Iceland. "Here is a sign of ice melting in action," continues Matthew, showing water flowing along the glacier's edge. "This valley glacier is retreating exceptionally rapidly, in fact equivalent of the length of a football field annually." The interview can be seen on the web together with the account of the visiting /about-imo/news/nr/1412