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Langjökull volcano

Stratovolcano volcano (subglacial) 1360 m (4,462 ft)
Iceland, 64.75°N / -19.98°W
Current status: dormant (1 out of 5)
Langjökull volcano books
Typical eruption style: Large effusive eruptions from  flank fissures, explosive activity from the summit crater.
Langjökull volcano eruptions: ca. 925 AD
TimeMag. / DepthDistanceLocation
Sat, 27 May
Sat, 27 May 04:43 UTCM 1.3 / 2 km15 km10.0 km WSW of Hveravellir
Sat, 27 May 04:43 UTCM 1.7 / 2.6 km18 km7.6 km W of Hveravellir
Fri, 26 May
Fri, 26 May 18:05 UTCM 1.6 / 4.3 km18 km9.0 km W of Hveravellir
Fri, 26 May 08:42 UTCM 1.6 / 3.3 km18 km8.1 km W of Hveravellir
Wed, 24 May
Wed, 24 May 01:16 UTCM 1.4 / 0.1 km27 km27.7 km WNW of Hveravellir
View all recent quakes
The Langjökull central volcano lies at the northern end of an active volcanic zone that extends to the NE from the Reykjanes Peninsula.

Background:

Langjökull volcano occupies the NE half of the massive Langjökull icecap, east of the prominent Pleistocene table mountain, Erikskökull. A summit caldera lies beneath the ice. Several shield volcanoes have been constructed along flank fissure zones, and postglacial lava flows flank Langjökull on the northern, western, and eastern sides. One of the most prominent of these is a small shield volcano that was formed at the site of the massive Hallmundahraun lava flow, which covers 200 sq km, and was erupted shortly after 900 AD.
The Geysir thermal area, containing Iceland's largest geysers, lies in the Haukadalur basin, near the southern end of the lengthy fissure system extending from Langjökull central volcano.
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Source: GVP, Smithsonian Institute


Latest satellite images


Background

The Langjökull central volcano lies at the northern end of an active volcanic zone that extends to the NE from the Reykjanes Peninsula.
Langjökull volcano occupies the NE half of the massive Langjökull icecap, east of the prominent Pleistocene table mountain, Erikskökull. A summit caldera lies beneath the ice. Several shield volcanoes have been constructed along flank fissure zones, and postglacial lava flows flank Langjökull on the northern, western, and eastern sides. One of the most prominent of these is a small shield volcano that was formed at the site of the massive Hallmundahraun lava flow, which covers 200 sq km, and was erupted shortly after 900 AD.
The Geysir thermal area, containing Iceland's largest geysers, lies in the Haukadalur basin, near the southern end of the lengthy fissure system extending from Langjökull central volcano.


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Source: GVP, Smithsonian Institute



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