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• 11. News

  as white dots, 20-26 October as red dots and 23-25 October as green dots. The M5.6 event is marked as a black star. The blue circle shows the area of the cluster that was detected 23-25 October further east of the main cluster. Tectonic faults are shown as black lines. News 2023 /about-imo/news/bigimg/2561

• 12. News

  stars, manually revised aftershocks are shown as red circles. The M5.5 mainshock is located on a north-south striking left lateral strike-slip fault (see red and white symbol). Earthquakes from 1992-2012 are shown as black dots (black lines are mapped faults). Click to enlarge. News /about-imo/news/bigimg/2685

• 13. HaBj_PlumePictures_w_explanations-20140901

  it easily discernible. (Photo: Halldór Björnsson) The plume rises from the vent but eventually reaches a level of neutral buoyancy and forms a white wrinkled eruption cloud. Near this level a dark shadow can be seen. In eruptions plumes such dark spots are often a sign of ash, but they can also be simply regular shadows. A detailed inspection revealed no ash falling from the cloud at this level. (Photo /media/jar/myndsafn/HaBj_PlumePictures_w_explanations-20140901.pdf

• 14. News

  24th September - 3rd October 2013. Black stars are earthquakes over 3 in magnitude off the firth of Eyjafjörður in 2013. The black and white spheres are solutions for a few of the 2013 quakes, all showing right-hand movement in concordance with the right lateral transform zone of the Húsavík-Flatey fault (HFF) shown by arrows off Flateyjarskagi. The broad arrows at the upper section of the map /about-imo/news/bigimg/2760

• 15. Solar eclipse on 1st August

  In Akureyri the eclipse begins at 08:17 GMT. and ends at 10:14 GMT. At its peak, the eclipse will cover 62% of the sun's diameter. People should avoid looking directly into the sun without using very dark glasses or film. The safest way to watch the eclipse is to let a binocular or monocular project the sun's image onto white cardboard, and then adjust the focus for sharpness. For further /about-imo/news/nr/1363

• 16. News

  2010, as seen at 12:00 GMT at an elevation of 3-3.6 km (10-12,000 ft). Light coloured, low-lying clouds of steam were observed over the eruption site, together with occasional bursts of grey to black-coloured cloud, which rise to up to half of the total height of the eruption plume. Above this level, the plume was lighter in colour with a capping of white cloud (not visible here /about-imo/news/bigimg/1891

• 17. Eyjafjallajokull_status_2010-05-24_IES_IMO

  images and web-based ash reports from the public. 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: Low discharge from Gígjökull. Conditions at eruption site /media/jar/Eyjafjallajokull_status_2010-05-24_IES_IMO.pdf

• 18. Seismic swarm near Grímsey: update 15:00, 19 February

  show the locations of earthquakes since January 2018. Earthquakes with magnitude larger than 4 are shown as black stars and the white star indicates the location of the M5.2 earthquake. The beachball (black/white ball) shows its focal mechanism, normal faulting. Grey dots show seismicity over the period 1994-2017. The brown lines show the Húsavík fault on-land and the black arrows /about-imo/news/seismic-swarm-near-grimsey-update-15-00-19-february

• 19. Update on activity in Eyjafjallajökull 2010

  were white and contained little or no ash. Details in a status report issued collectively by the Icelandic Meteorological Office and the Institute of Earth Sciences today at 15:00. The volcano is still monitored closely. Ash mist over Reykjavík Friday 4 June 2010 wind blew loose ash from Eyjafjallajökull across south- and southwest Iceland. Reykjavík is invisible across the small bay /earthquakes-and-volcanism/articles/nr/1884

• 20. ice-chart_colour-code-standard

  for ice charts only dealt with black and white charts, in keeping with the paper facsimile technology of the time, colour has long been used to help differentiate the various ice conditions on a paper chart. In the last decade, progress in computer processing and communication, as well as increased demands of users prompted the necessity to develop a new WMO International Ice Colour Code Standard /media/hafis/frodleikur/ice-chart_colour-code-standard.pdf