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News
Map of recent quakes under Torfajökull (Iceland Met Office)
Sunday, Feb 17, 2013
Un enjambre de pequeño terremoto ha comenzado hoy. Incluye unos 20 sismos de pequeña magnitud a profundidades someras de 2-4 km. ... [Leer más]

 

Torfajökull volcano

Stratovolcano 1259 m / 4,131 ft
Iceland, 63.93°N / -19.18°W
Current status: normal or dormant (1 out of 5) | Reports
Torfajökull volcano books
Last update: 16 May 2018 (earthquake swarm)
Typical eruption style:

Effusive and explosive.


Erupciones del volcán Torfajökull: ca. 900 AD, 1170(?), 1477
Fecha / HoraRevista / ProfundidadDistanciaUbicación
Sat, 23 Mar 2019
Sat, 23 Mar 06:53 UTCM 0.7 / 0.1 km2 km7.7 km NE of Hábunga (Iceland)
Sat, 23 Mar 06:43 UTCM 1.2 / 0.1 km1 km6.4 km NNE of Hábunga (Iceland)
Sat, 23 Mar 06:43 UTCM 0.8 / 1.1 km2 km5.6 km NE of Hábunga (Iceland)
Sat, 23 Mar 00:46 UTCM 1.7 / 21.2 km1 km7.0 km NNE of Hábunga (Iceland)
Sat, 23 Mar 00:46 UTCM 0.7 / 1.1 km10 km3.1 km S of Goðabunga (Iceland)
Ver los sismos recientes
The Torfajökull central volcano, located north of Myrdalsjökull and south of Thorisvatn lake, is cut by a 12-km-wide caldera that formed during the Pleistocene.

Background:

Torjajokull consists of the largest area of silicic and intermediate volcanism in Iceland; about 225 cu km of silicic extrusive rocks are exposed. The dominantly rhyolitic complex rises about 500 m above surrounding basaltic plains and is elongated in a WNW-ESE direction. Most rhyolitic lava flows were erupted subglacially, forming silicic hyaloclastites that form ridge and dome-shaped breccias.

During postglacial times only a narrow fissure zone at the western end has been active, producing mostly silicic lava flows, lava domes, and tephras. The most recent silicic eruption produced the Hrafntinnuhraun lava flow about 900 AD. The fissure system is along trend with and was active at the same time as the basaltic Veidivötn fissure system of Bárdarbunga central volcano in 1477 AD. The small Torfajökull icecap lies mostly outside the SE rim of the caldera, which is the site of vigorous thermal activity over a broad area of 130-140 sq km.

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Source: GVP, Smithsonian Institute


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