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• 21. Eyjafjallajokull_status__2010-04-25_IES_IMO

  at 5.3 km. Heading: NW Colour: No information Tephra fallout: Minor (light fallout detected at two farms 10 km NW of vents) Meltwater: 100-120 m3/s, based on gauge at old Markarfljót bridge and a rough estimate of base flow. Conditions at eruption site: Overall activity similar as yesterday. Eruption seen from west in the morning - north crater still active. External water has /media/jar/Eyjafjallajokull_status__2010-04-25_IES_IMO.pdf

• 22. norsem_bryndis

  Crustal accretion along the divergent plate boundary in Iceland is governed by rifting episodes and dyking. Over a period of two weeks in August-September 2014, magma propagated laterally from the subglacial Bárðarbunga central volcano, Iceland, about 50 km along the divergent plate boundary to the NNE where it erupted continuously for six months. The dyke propagation was associated with more /media/norsem/norsem_bryndis.pdf

• 23. norsem_lund

  more events in the vicinity in the next two months. These aftershocks are interesting as aftershocks to M4+ events are not always observed in Sweden and Finland. The Bothnian Bay is one of the most seismically active areas in continental Fennoscandia, but the cause of the seismicity is still not well known. Until recently, the offshore areas have been poorly monitored by the national seismic /media/norsem/norsem_lund.pdf

• 24. Eyjafjallajokull_status_2010-04-29_IES_IMO

  from the local police; and aerial observations from a scientific flight with the Icelandic Coastguard (observation plane TF-SIF). Eruption plume: Height (a.s.l.): Not visible above clouds at 3.6–5.1 km (12–17,000 ft), but most likely below 3.6 km (12,000 ft). Before the overflight this morning, the eruption plume was not seen on radar images from Keflavík, nor on satellite /media/jar/Eyjafjallajokull_status_2010-04-29_IES_IMO.pdf

• 25. Ash measurements

  the National Centre for Atmospheric Science (NCAS) in the UK. The instrument transmits laser beams into the atmosphere and measures the light that is backscattered towards the ground. The instrument was installed on the lowlands close to the volcano Eyjafjallajökull which erupted last year. The aim was to measure windblown resuspended ash from last year's eruption. Following the eruption at Grimsvotn /about-imo/news/nr/2183

• 26. Bárðarbunga earthquakes 3D

  of earthquakes in Bárðarbunga 16 - 26 August 2014. IMO's specialist, Bogi B. Björnsson, compiled this video from the available data. 16 - 20 August 2014 The Bárðarbunga seismic activity can now be explored in a three dimensional video (30 sec.) which shows earthquakes from 16th to 20th August 2014. Location, depth and age of earthquakes in Bárðarbunga 16-20 August 2014. The colour /earthquakes-and-volcanism/articles/nr/2948

• 27. Eyjaf_status_2010-05-04_IES_IMO

  The plume has also been observed on IMO's weather radar at 5.2-5.4 km height between 13:05 and 14:00 GMT. Heading: East-south-east to south-east from the eruption site. Plume track clearly visible up to 300-400 km distance from the eruption site on a noaa satellite image at 13:13 GMT. Colour: Observation from web cameras and from pilots in ICG-flight: Dark grey ash plume observed over the eruptive /media/jar/Eyjaf_status_2010-05-04_IES_IMO.pdf

• 28. Eyjafjallajokull_status_2010-06-07_IES_IMO

  June. In the western part of the crater, a new crater has formed at the site of explosive activity. Tremor pulses late 6 June accompanied steam plumes from this new crater. The plumes and explosions are small. Caving in of lava in the conduit can be heard between explosions. Only a part of the new active crater has been seen due to the steam. The glacial ice at the top is advancing rapidly /media/jar/Eyjafjallajokull_status_2010-06-07_IES_IMO.pdf

• 29. Eyjafj_status_2010-04-27

  the air at 12:00 GMT at an elevation of 3–3.6 km (10–12,000 ft). Heading: West–northwest from the eruption site. Colour: Light, low-lying clouds of steam observed over the eruption site, together with occasional bursts of grey to black-coloured cloud, which rose 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 /media/jar/myndsafn/Eyjafj_status_2010-04-27.pdf

• 30. VI_2009_013

  to locate earthquakes in Iceland but the SIL-crustal model has no Moho boundary. Using this model in the routine, daily analysis, the majority of the earthquakes in Eyjafjallajökull form a 3-km-wide chimney between 1 and 10 km depth beneath the northern flank of the volcano. A smaller cloud is also visible between 19 and 25 km depth, about 1.5 km west of the main activity/cluster. 13 Figure 3 /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf