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Zufallsfotos

Nachrichten:

Tuesday, Feb 18, 2020
The Icelandic Met Office (IMO) recorded an earthquake swarm since 15 February at the southwestern tip of the Reykjanes peninsula. Over 120 earthquakes were detected by the seismic network with magnitude below M 3.0. ... [mehr]
Depth vs time of earthquakes beneath Thornbjorn volcano during the past days
Saturday, Feb 08, 2020
Earthquake activity around Thornbjorn volcano has decreased over the past days, but weak inflation, likely caused by magma accumulation at shallow depth, continues. ... [mehr]
 

Reykjanes Vulkan

Crater rows 230 m / 755 ft
Reykjanes peninsula (SW Iceland), 63.89°N / -22.52°W
Aktueller Status: unruhig (2 von 5)
Reykjanes Webcams / aktuelle Daten | Berichte
Reykjanes Vulkan-B cher | Tours
Last update: 18 Feb 2020 (seismic swarm)
Typische Aktivität: effusive (lava flows)
Ausbrüche des Reykjanes: 1211, 1226
UhrzeitMag. / TiefeDistanceOrt
Tue, 18 Feb 2020
Tue, 18 Feb 09:14 UTCM 0.5 / 5.6 km8 km5.9 km NNE of Reykjanestá (Iceland)
Tue, 18 Feb 08:37 UTCM 1.5 / 5.6 km11 km3.5 km N of Reykjanestá (Iceland)
Tue, 18 Feb 08:17 UTCM 1.0 / 5.3 km7 km6.7 km NNE of Reykjanestá (Iceland)
Tue, 18 Feb 07:55 UTCM 1.6 / 7.6 km5 km2.4 km NNW of Grindavík (Iceland)
Tue, 18 Feb 06:04 UTCM 0.7 / 6.9 km7 km7.1 km NNE of Reykjanestá (Iceland)
Alle anzeigen
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.

Beschreibung:

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

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