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Map of recent quakes near Askja
Mittwoch, Mär 27, 2013
Small earthquakes have also been more frequent under and near the Askja caldera and Bardabunga volcano (to the SW of Askja) in the past few days. [mehr]
Location of recent quakes near Askja
Sonntag, Mär 10, 2013
A swarm of earthquakes at shallow depths, mostly around 2-5 km has been occurring in an area about 12 km NE of the caldera. 27 quakes including 6 between magnitudes 2.1-2.7 were recorded yesterday. [mehr]

Askja Vulkan

Schichtvulkan 1516 m (4,974 ft)
Central Iceland, 65.03°N / -16.75°W
Aktueller Status: unruhig (2 von 5)
Askja Webcams / aktuelle Daten
Letztes Update: 27 Mär 2013
Typische Aktivität: explosive + effusive
Ausbrüche des Askja : 1797(?), 1875, 1919, 1921, 1922, 1923, 1924(?), 1926, 1938, 1961
Letzte Erdbeben in der Nähe:
ZeitMag. / TiefeDistanceOrt
Wed, 19 Jun
Wed, 19 Jun 12:51 UTCM 0.6 / 9.6 km15 km18.1 km NNW of Kverkfjöll
Wed, 19 Jun 12:50 UTCM 1.1 / 12.7 km15 km18.1 km NNW of Kverkfjöll
Wed, 19 Jun 12:50 UTCM 1.6 / 9.5 km15 km17.9 km NNW of Kverkfjöll
Wed, 19 Jun 08:05 UTCM 0.6 / 3 km3 km4.1 km WSW of Dreki
Wed, 19 Jun 07:52 UTCM 1.5 / 6.8 km23 km2.9 km NW of Kistufell
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Askja is a large basaltic central volcano that forms the Dyngjufjöll massif. It is truncated by three overlapping calderas, the largest of which is 8 km wide and may have been produced primarily from subglacial ring-fracture eruptions rather than by subsidence.

Beschreibung:

A major rhyolitic explosive eruption from Dyngjufjöll about 10,000 years ago was in part associated with the formation of Askja caldera. Many postglacial eruptions also occurred along the ring-fracture. A major explosive eruption on the SE caldera margin in 1875 was one of Iceland's largest during historical time. It resulted in the formation of a smaller 4.5-km-wide caldera, now filled by Öskjuvatn lake, that truncates the rim of the larger central caldera. The 100-km-long Askja fissure swarm, which includes the Sveinagja graben, is also related to the Askja volcanic system, as are several small shield volcanoes such as Kollatadyngja. Twentieth-century eruptions at Askja have produced lava flows from vents located mostly near Öskjuvatn lake.

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Source: GVP, Smithsonian Institution



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