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Bárdarbunga Vulkan
Stratovolcano approx. 2000 m / ca. 6,560 ft
Central Iceland, 64.63°N / -17.53°W
Aktueller Status: normal / ruhend (1 von 5)
Bárdarbunga Webcams / aktuelle Daten | Berichte
Bárdarbunga Vulkan-B cher
Ausbrüche des Bárdarbunga :
1080(?), 1159(?), ca. 1210, ca. 1270, ca. 1350, ca. 1410(?), 1477 (very large effusive-explosive eruption), 1697, 1702, 1706, 1712, 1716, 1717, 1720, 1726, 1729, 1739, 1750, 1766, 1769, 1797, 1807(?), 1862-64, 1872(?), 1902-03
Typische Aktivität:
Large effusive eruptions, some explosive activity.
Letzte Erdbeben in der Nähe
Letzte Satellitenbilder

Bárdarbunga Vulkan: Nachrichten

Bardarbunga volcano update: Holuhraun eruption continues

Monday Sep 01, 2014 07:57 AM | VON: T

Picture of the eruption this morning (image: Gísli Einarsson / RUV)
Picture of the eruption this morning (image: Gísli Einarsson / RUV)
Earthquakes since midnight (IMO
Earthquakes since midnight (IMO
The fissure eruption is continuing at a stable level with little variation. A curtain of lava fountains up to 70 m high is being erupted above the fissure and pahoehohoe type lava flows are expanding to several kilometers around it, forming a growing flat lava flow field.
The effusion rate along the fissure vent has been estimated to be up to an impressive 1000 cubic meters per second.
Update from IMO this morning:
"No explosive activity is observed, the eruption remains an effusive lava eruption. Visual observation by webcam and low level volcanic tremor on seismometers do not show any obvious changes since evening.

Seismic activity:

Around 250 earthquakes have been automatically detected until now. Most of them are located in the northern part of the magma intrusion, between the eruption site and south to about 10 km into Dynjujökull. Strongest events were up to around magnitude 2. The rate of events has decreased as a result of pressure release due to the eruption, but there is still ongoing continuous seismicity.

Several events have occurred around the Bárðarbunga caldera rim, strongest events were M4.2 at 03:09 on the southern rim and M4.5 at 04:59 on the northern rim. See maps.

In the broader Askja region, most events were located at Herðubreiðartögl, the strongest event there was M2.9 at 02:56. This area is a quite common place for seismic activity, the activity now is not necessarily caused by increased stress due to the intrusion (the tip of the intrusion is about 25 km SW of this cluster). Askja volcano itself was seismically quiet."
Vorherige Nachrichten
Sunday, Aug 31, 2014
According to local news, the lava flows have already reached more than 3 km distance from the fissure vent. The eruption is much stronger than the previous one on Friday, with up to 10 times lava output. ... [mehr]
Sunday, Aug 31, 2014
According to IMO, "the new eruption started in Holuhraun shortly after 04 AM, on the same volcanic fissure, which erupted earlier this week. The fissure is estimated to be 1,5 km long. ... [mehr]
View of the eruptive fissure this morning (Mila webcam 2)
Sunday, Aug 31, 2014
A new eruptive phase has started at the same fissure that had been briefly active Friday morning. ... [mehr]
The image shows earthquakes and GPS-displacements together in one picture. The earthquakes have different colours representing how long it's been since they were measured. GPS displacements are shown with black arrows. The circles around the arrows represent uncertainty in the measurements.
Saturday, Aug 30, 2014
The Icelandic Met Office has published two maps showing the (ongoing) mostly horizontal deformation, as evidenced by GPS measurements, in the Bardarbunga area during the past 3 days as well as since the beginning of the crisis. In just 2 weeks, the distance between the DYNC station (western side of the rift) and GSIG (eastern side) has increased by almost 50 cm! [mehr]
Location of today's earthquakes near Bardarbunga volcano (IMO)
Saturday, Aug 30, 2014
The still intense earthquake swarm and deformation continues with little variation. No further eruptive activity has occurred since yesterday's "blitz" eruption. ... [mehr]

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