Eyjafjallajökull

Català: Eyjafjallajökull és la cinquena glacera més gran d'Islàndia. Es troba al nord de la regió d'Skógar i a l'oest d'una glacera de major mida Mýrdalsjökull. La capa de glaç de la glacera cobreix el volcà (del mateix nom que la glacera).

Deutsch: Eyjafjallajökull ist ein subglazialer Vulkan im Süden von Island. Seine letzten Ausbrüche fanden im Jahr 2010 statt.

English: Eyjafjallajökull is a subglacial volcano in the south of Iceland. The latest eruptions were in 2010.

Français : Eyjafjallajökull est un volcan sous-glaciaire dans le sud de l' Islande. Ses dernières éruptions furent en 2010.

Македонски: Ејафјадлајекидл

Русский: Эйяфьядлайёкюдль — подледникового вулкан на юге Исландии.

Pronounciation

Pronunciation

Maps and satellite pictures

One of the southernmost volcanoes of Iceland
Ash plume
Earthquakes indicating the second eruption series under Eyjafjallajökull in 2010 (source:IMO)
Eyjafjallajökull is part of the EVZ (East Volcanic Zone)

Approaching Eyjafjallajökull

Aerial views

To the right of Mýrdalsjökull/Katla
The aircraft here is over Mýrdalsjökull, Eyjafjallajökull in front and behind it to the right, the volcanic archipelagos of the Westman Islands (Vestmannaeyjar)
Þórsmörk with the glacial river Krossá in the foreground

From the archipelagos of Vestmannaeyjar

With a Danish inspection vessel in the foreground

From Mýrdalsjökull

Views of the glacier and dormant volcano

Volcanic eruptions in 2010

Fimmvörðuháls eruptions in March - April 2010

The first series of eruptions started in March 2010 and went on for about 3 weeks. The effusive eruptions on the mountain pass Fimmvörðuháls originated in volcanic fissures which are part of the Eyjafjallajökull volcanic system.

2010-04-01: aerial view of the vents (NASA)
2010-03-25: The first pyroclastic cone and the steam cloud from the lava flow in Hrunagil. Seen from Fauskheiði.
2010-03-25: eruptions begin in the Fimmvörðuháls pass area
2010-03-27: Fimmvörðuháls in the twilight
2010-03-29: The first fissure that opened on Fimmvörðuháls, as seen from Austurgígar.
2010-04-02: steaming second fissure on Fimmvörðuháls
2010-04-03: on Fimmvörðuháls
2010-04-03: on Fimmvörðuháls
Aerial views of the Fimmvörðuháls eruptions

Eyjafjallajökull subglacial eruptions in April - June 2010

The second series of eruptions started subglacially under Eyjafjallajökull himself the 14th of April 2010 and went on til the end of June. They were explosive, producing very fine grained tephra of a trachyandesite type which caused important disruptions of European airtravel during the next weeks and months.

Cross cutting through the neighbouring Eyjafjöll and Katla volcanic systems with indication of the eruption locations
Scheme of a subglacial eruption. 1. Water vapor cloud, 2. Lake, 3. Ice, 4. Layers of lava and ash, 5. Stratum, 6. Pillow lava, 7. Magma conduit, 8. Magma chamber, 9. Dike

2010-04-17: The ash plume from the second eruption in Eyjafjallajökull seen from Fljótshlíð 1
2010-04-17: ash plume from the erupting Eyjafjallajökull 2
2010-04-17: ash plume from the erupting Eyjafjallajökull 3
2010-04-20: The second eruption in Eyjafjallajökull seen from Fljótshlíð at night.
2010-04-15: The craters at beginning of second eruption series
2010-05-01: ash plume from the erupting Eyjafjallajökull seen from the Falcon scientific airplane

Air travel disruptions in Europe

Satellite images of ash distribution

Ash plume on April 17, 2010
April 17, 2010
Ash plume over the North Atlantic, April 15, 2010
May 10, 2010
Volcanic ash over Europe on April 16, 2010

Situation at some airports

At Charles de Gaulle airport in Paris
At Leed Bradford Airport

Developments re. airtravel between 17th and 20th April 2010

April 18, 2010
April 19, 2010
April 20, 2010

Before and after

Gígjökull

Eyjafjallajökull's outlet glacier Gígjökull in 2003 with the glacial lake in front
Outlet glacier in 2004
Outlet glacier and lake in 2007 (before the eruptions)
Gígjökull during the eruptions in May 2010
The same outlet glacier in 2011 after the eruptions
Also in 2011: The lake has not only disappeared, but has been replaced by a hill of volcanic ash and debris...
... placed there during jökulhlaup and eruption of lava flows, which trickled beneath the glacier down to the valley