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The image shows the two eruption sites, Eyjafjallajökull that started 14 April, and Fimmvörðuháls 20 March to 12 April. © NASA Earth Observatory.
The image shows the two eruption sites, Eyjafjallajökull that started 14 April, and Fimmvörðuháls 20 March to 12 April. © NASA Earth Observatory.


Latest news:

Eyjafjallajøkull volcano (Iceland): low activity resumes
mercredi, juin 09, 2010
Eyafjallajokull's eruption might not yet have ended or be ending yet. The vent in the western crater still produces small magma explosions and some as... [details]
Eyjafjallajøkull volcano (Iceland): activity has stopped
lundi, mai 24, 2010
It seems that the eruption of Eyafjallajökull volcano has finally ended. While ther is stilla considerable steam plume rising from the crater, no fres... [details]

Eyafjallajökull volcan

stratovolcan 1666 m (5,466 ft)
Islande, 63.63°N / -19.62°W
Condition actuelle: en sommeil (1 sur 5)
Eyafjallajökull webcams / live data
Style éruptif tipique: Effusive (Hawaiian-style lava fountains and lava flows), mildly explosive due to ice-water-lava interaction.
Eruptions du volcan Eyafjallajökull: 1821-23, 20 March - June 2010 The ash cloud from erupting Eyafjallajökull volcano, which spread over Europe in mid April and led to an unprecedented closure of airspace for almost 7 days over almost all of Europe
Eyafjallajökull photos du volcan
Eyafjallajökull volcano (its name meaning Island-Mountain under a glacier) under the small homonymous glacier in southern Iceland erupted spectacularly on 20 March 2010, after having been dormant for almost 200 years. During its most violent phase, the subglacial eruption produced large ash plumes that drifted over Europe and forced an unprecedented closure of airspace over most of Europe for several days in mid April 2010.

Introduction:

Eyjafjöll, located immediately west of Katla volcano, consists of an E-W-trending, elongated ice-covered basaltic-andesite stratovolcano with a 2.5-km-wide summit caldera.
Fissure-fed lava flows occur on both the eastern and western flanks of the volcano, but are more prominent on the western side. Although the 1666-m-high volcano has erupted during historical time, it has been less active than other volcanoes of Iceland's eastern volcanic zone, and relatively few Holocene lava flows are known. The sole historical eruption of Eyjafjöll, during December 1821 to January 1823, produced intermediate-to-silicic tephra from the central caldera.
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Source: GVP, Smithsonian Institute

Eyafjallajökull Photos:

The ash plume generated by Eyafjallajökull's eruption in April 2010. (Photo: Jorge Santos)
The ash plume generated by Eyafjallajökull's eruption in April 2010. (Photo: Jorge Santos)