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Actualités:


dimanche, oct. 13, 2013
A shallow (10 km) magnitude 4.8 earthquake with many pre- and aftershocks (or a seismic swarm) occurred this morning (Sun) at 07:34 UTC at the SW tip of the Reykjanes peninsula, on the SW active rift zone. The swarm of earthquakes included several quakes of magnitude 3 and higher. The strongest earthquake was widely felt in SE Iceland. ... [details]
Earthquakes on and around Iceland on 30 Aug - the Kolbeinsey Ridge is the area with the yellow dots to the north (map: Icelandic Met Office)
vendredi, août 31, 2012
Yesterday, there was a lot of earthquake activity on Iceland. At noon, a swarm with about 50 quakes partly preceded and followed a magnitude 4.2 quake at 5.8 km depth beneath the Reykjanes peninsula, near the axis of the the SW volcanic rift zone. Most quakes were between magnitudes 1-2 and at around 5 km depth. ... [details]
 

Reykjanes volcan

Rangées Cratère 230 m / 755 ft
Reykjanes peninsula (SW Iceland), 63.89°N / -22.52°W
Condition actuelle: normal / en sommeil (1 sur 5) | Reports
Reykjanes livres | Tours
Last update: 13 oct. 2013
Style éruptif tipique: effusive (lava flows)
Eruptions du volcan Reykjanes: 1211, 1226
HeureMag. / DepthDistanceLocation
Tue, 11 Dec
Tue, 11 Dec 17:02 UTCM 1.3 / 6.3 km10 km4.1 km SW of Fagradalsfjall
Tue, 11 Dec 17:02 UTCM 1.7 / 7.8 km11 km4.0 km SSW of Fagradalsfjall
Tue, 11 Dec 16:47 UTCM 2.2 / 7.1 km10 km4.4 km N of Reykjanestá
Tue, 11 Dec 16:16 UTCM 1.3 / 9.7 km5 km3.6 km ENE of Fagradalsfjall
Tue, 11 Dec 11:35 UTCM 1.7 / 7.7 km11 km3.4 km SSW of Fagradalsfjall
Voir tous
Reykjanes volcano in SW Iceland is located where the Mid Atlantic Ridge emerges onto land. It forms a vast area with many eruptive fissures, lava fields, hot springs and mud pools. In 2000, a large earthquake lowered the water level in Lake Kleifarvatn by 5 metres, but has gradually returned to normal since then.

Introduction:

The Reykjanes volcanic system at the SW tip of the Reykjanes Peninsula, where the Mid Atlantic Ridge rises above sea level, comprises a broad area of postglacial basaltic crater rows and small shield volcanoes.
The Reykjanes volcanic system is the westernmost of a series of four closely-spaced fissure systems that extend diagonally across the Reykjanes Peninsula. Most of the volcanic system is covered by Holocene lavas and eruptions have occurred in historical time during the 13th century at several locations on the NE-SW-trending fissure system.
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Source: GVP, Smithsonian Institute

Reykjanes Photos:




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