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• 61. 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

• 62. VI_2009_013

  mechanisms and the relationship between b-values and source depth is examined. During the analysis period, three major swarms were recorded. Two of the swarms, in 1994 and 1999–2000, occurred in the upper crust and were accompanied by crustal deformation. No uplift was detected during the third swarm, which occurred in 1996 near the crust mantle boundary, between 19 and 25 km depth /media/vedurstofan/utgafa/skyrslur/2009/VI_2009_013.pdf

• 63. Kok_JGEC658_2009

  /media/loftslag/Kok_JGEC658_2009.pdf

• 64. On the Bárðarbunga gradual caldera collapse

  volcano collapsed during the eruption as 1.9 km³ of magma flowed laterally from a magma reservoir under the volcano. About one quarter formed a 48 km long dyke (0.5 km³) while about three quarters were erupted in Holuhraun (1.4 km³) over the six months between 31 August 2014 and 27 February 2015. The subsidence bowl formed in Bárðarbunga was up to 65 m deep and the area where subsidence exceeded 1 m /about-imo/news/on-the-bardarbunga-gradual-caldera-collapse

• 65. On the Bárðarbunga gradual caldera collapse

  volcano collapsed during the eruption as 1.9 km³ of magma flowed laterally from a magma reservoir under the volcano. About one quarter formed a 48 km long dyke (0.5 km³) while about three quarters were erupted in Holuhraun (1.4 km³) over the six months between 31 August 2014 and 27 February 2015. The subsidence bowl formed in Bárðarbunga was up to 65 m deep and the area where subsidence exceeded 1 m /about-imo/news/on-the-bardarbunga-gradual-caldera-collapse/

• 66. HARMONIE - numerical weather prediction model 

  convection-permitting NWP and is operated at 2.5 km horizontal resolution over a domain that covers Iceland and the surrounding seas. The development and maintainance of the model is a research cooperation of European meteorological institutes that was founded in 2005 when two research consortia joined forces. One of these consortium was the HIRLAM programme (High Resolution Limited Area /weather/articles/nr/3232

• 67. 2010-05-02_En-IES_IMO

  scientists at Gígjökull. [No scientific overflight today.] Eruption plume: Height (a.s.l.): Estimated from web-camera views and observers on the ground at an elevation of 4–5.4 km (13–18,000 ft). Clouds of ash at lower elevations observed drifting south-east of the eruption site. No verifiable detections from the weather radar at Keflavík Airport. Heading: South-east from /media/jar/2010-05-02_En-IES_IMO.pdf

• 68. Eyjafjallajokull_status_2010-05-14_IES_IMO

  and web-based ash reports from the public. Eruption plume: Height (a.s.l.): Mainly ~7 km / 24,000 ft. Heading: West and later southwest. Colour: Grey. Tephra fallout: Ashfall reported from the Vestmanna Islands, Rangárþing east and in Reykjavík. Lightning: More than 50 lightning strikes were recorded on the ATDnet during the last 24 hours. Between 4 and 5 this morning, 10 lightning were /media/jar/Eyjafjallajokull_status_2010-05-14_IES_IMO.pdf

• 69. Articles

  April 2010 at 10:43 which advanced at the speed of 5 km per hour. Related topics UNESCO USGS /hydrology/articles/bigimg/2097

• 70. Eyjafjallajökull

  volcanic system is located on the Eastern Volcanic zone, approximately 25 km west of Katla volcano. Eyjafjallajökull volcano is a 1666 m high stratovolcano with an east-west elongated direction, the system is about 25 km long and 15 km wide. The volcano is mostly covered by ice and has an ice-filled caldera of about 2.5 km wide.In the last 8000 years Eyjafjallajökul has been moderately active /volcanoes/about-volcanoes/eyjafjallajokull/