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• 31. The crater at Grímsvötn

  The volcanic tremor recorded from Grímsvötn has dropped significantly since yesterday (as shown on tremor plot below). The largest pulse of increased explosive activity was observed at around 02:00 AM last night. The eruption site was observed during a flight yesterday evening. The eruption plume was rather low (approx. 3 km high) and white when the flight arrived at Grímsvötn but at 20:55 /about-imo/news/nr/2188

• 32. The crater at Grímsvötn

  (approx. 3 km high) and white when the flight arrived at Grímsvötn but at 20:55 GMT explosive activity increased again and the plume rose to about 7.5 km height. The increased activity was observed for about 20 minutes, then the activity dropped down at 21:15 GMT and increased again at 21:45 GMT. This pulsating activity is also clearly seen on tremor plots (click to enlarge) from near seismic /about-imo/news/nr/2188/

• 33. Eyjafjallajokull_status_2010-05-23_IES_IMO

  data; web cameras, ATDnet – UK Met. Offices lightning detection system, Satellite images, web-based ash reports from the public and observations from aircraft. Eruption plume: Height (a.s.l.): According to a pilot, the plume is estimated at 3 km/10,000ft. A light northerly wind. Heading: South. Colour: White, steam. Tephra fallout: No reports of ashfall. Lightning: No lightning strikes have /media/jar/Eyjafjallajokull_status_2010-05-23_IES_IMO.pdf

• 34. Eyjafjallajokull_status_2010-05-25_IES_IMO

  detection system, Satellite images and web-based ash reports from the public, and scientist on the volcano. Eruption plume: Height (a.s.l.): According to a webcamera, the plume is estimated at 2 km/6600ft. A light northerly wind. Heading: South. Colour: White, steam. Tephra fallout: No reports of ashfall. Lightning: No lightning strikes have been detected. Noises: No reports. Meltwater /media/jar/Eyjafjallajokull_status_2010-05-25_IES_IMO.pdf

• 35. Eyjafjallajokull_status_2010-05-26_IES_IMO

  images and web-based ash reports from the public. Eruption plume: Height (a.s.l.): According to a webcamera in the morning, the plume was estimated at 2 km/6600ft. Northerly wind. Heading: South. Colour: White, steam. Tephra fallout: No reports of ashfall. Lightning: No lightning strikes have been detected. Noises: No reports. Meltwater: Low discharge from Gígjökull. Conditions at eruption site /media/jar/Eyjafjallajokull_status_2010-05-26_IES_IMO.pdf

• 36. Eyjafjallajokull_status_2010-06-01_IES_IMO

  system, web- based ash reports from the public and scientists that went to the volcano. Eruption plume: Height (a.s.l.): Clouds and mist have covered the summit of the volcano both yesterday and today. At 08:00 GMT today a white cloud was seen at 2 km a.s.l. on web-cameras. Winds of up to 10 m/s are blowing from the east. Heading: N/A Colour: N/A Tephra fallout: Widespread drifting /media/jar/Eyjafjallajokull_status_2010-06-01_IES_IMO.pdf

• 37. Kok_and_Veldkamp_editorial_ES-2011-4160

  the notion of complex systems, specifically the social-ecological system, is needed to improve the understanding of scale and governance. They furthermore confirm that both communities are shifting. Additionally, the papers show several promising ways forward to link scale and governance, even though they differ in their suggestions on most important courses of action and research agendas. The case /media/loftslag/Kok_and_Veldkamp_editorial_ES-2011-4160.pdf

• 38. 2010-05-02_En-IES_IMO

  the eruption site. Plume track visible at least 200 km from the eruption site on MODIS (12:35 GMT) and EUMETSAT (17:15 GMT) satellite imagery. Colour: Dark grey (ash) clouds observed over the eruptive site. White (steam) plumes rising from Gígjökull, north of the eruption site. Tephra fallout: Moderate ash-fall reported in the village of Vík (12:00 GMT), located 40 km south-east /media/jar/2010-05-02_En-IES_IMO.pdf

• 39. Grímsey earthquake swarm

  are indicated as black stars and earthquakes with a magnitude over 4 as white stars. Grey dots show earthquake activity in 1994-2017. Black triangles show the location of seismic stations and the black arrows show the movement across the Húsavík Flatey fault. Figure below:Displacements of the GPS station in Grímsey in mm for North, East and Up directions are shown as a time series for the past /about-imo/news/grimsey-earthquake-swarm

• 40. On the Askja rockslide

  at the lakeshore who might not have been able to escape the tsunami. There were no eyewitnesses to the slide, but members of a search- and rescue team saw a white plume rise up above Askja at 23:27. The steam plume was created when the slide exposed shallow geothermal areas in the release area. In addition, a dust cloud created by the rock slide may have contributed to the plume. Askja consists /about-imo/news/nr/2930