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Aug 20 2014 08:17am
Bardarbunga volcano in iceland seems to be poised for an eruption
things could get interesting soon

This post was edited by low-ki on Aug 20 2014 08:19am
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Aug 23 2014 01:17pm
link won't show, but type volcanocafe into google or w/e..good site to keep up to date

it's has started

This post was edited by low-ki on Aug 23 2014 01:24pm
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Aug 24 2014 12:55am
from the official site = http://www.almannavarnir.is/displayer.asp?cat_id=133

23.08.2014
t 14:00 UTC, an over-flight was made to Bárðarbunga by the Icelandic Coastguard with scientists from the Icelandic Meteorological Office and the University of Iceland, in addition to a representative from the National Commissioner of the Icelandic Police.
The over-flight covered the north-western region of the Vatnajökull ice-cap in clear conditions. Both visual observations and radar measurements confirmed no significant changes on the surface of Vatnajökull. Likewise, there were no signs of floodwater draining from the ice margin.
During three hours of aerial surveillance, there were no obvious signs of volcanic activity.
In light of the intense, ongoing earthquake activity and crustal deformation at Bárðarbunga, the Icelandic Meteorological Office has decided that the aviation colour-code should remain ‘red’. The situation will be reassessed tomorrow morning
The National Commissioner of the Icelandic Police in collaboration with the District Commissioners of Police in Húsavík and Seyðisfjörður has decided that the emergerncy phase will stay in effect. The decision will be evaluated at noon tomorrow 24 August.


which is in about 5 hours from now
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Aug 24 2014 06:19am
24.08.2014 at 11:40 UTC

Earthquake activity in NW-Vatnajökull is still very strong, 700 earthquakes have been observed since midnight and they are somewhat larger than previous days.
Two large earthquakes, over 5 where in the Bárðarbunga caldera this night.
The activity under Dyngjujökull has propagated northwards and is now mostly under the edge of the glacier, where an earthquake of size 4,2 was recorded this morning.
The dyke under Dyngjujökull is now estimated to be approximately 30 km long.
There are no indications that the activity is slowing down, and therefore an eruption can not be excluded.
Observations show that a sub-glacial eruption did not occur yesterday. The intense low-frequency seismic signal observed yesterday has therefore other explanations.
The Icelandic Meteorological Office has decided to move the aviation color-code from red to orange
.
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Aug 24 2014 03:49pm
CAM1: Bardarbunga (front of the cam), Iceland
[private camera, no link]

CAM2: Kverkfjöll, Iceland (delayed)
http://vedur2.mogt.is/kverkfjoll/webc...

CAM3: Bardarbunga, Iceland (live)
http://www.livefromiceland.is/webcams...

Earthquake Map
http://en.vedur.is/#tab=skjalftar

Crustal Deformations GPS measurements
http://strokkur.raunvis.hi.is/gps/#VATN

3D Earthquake Map
http://baering.github.io/

Sounds of Bardarbunga
http://halldorel.github.io/

Dynamic Tremors
http://hraun.vedur.is/ja/oroi/dyn.gif
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Aug 27 2014 09:12am
Carl Sagan approves this message.
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Aug 28 2014 07:22pm


it started ...so far just a 5 mile wide fissure opened up...
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Aug 31 2014 07:38am
2nd fissure has opened now
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Aug 31 2014 08:19am
iceland and their damn volanoes

Papua New Guinea too

This post was edited by KvoStava on Aug 31 2014 08:20am
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Sep 10 2014 03:36am
"Gravely concerned" about Bardarbunga

Fyrst birt: 09.09.2014 22:00, Síðast uppfært: 09.09.2014 22:00

Increased subsidence in the caldera of Bardarbunga volcano is a cause for grave concern, due to possible large eruption and glacial flood, says Vidir Reynisson, director of the Civil Protection Agency in Iceland. The subsidence is thought to increase the likelyhood of an eruption in Bardarbunga.


An ongoing lava eruption, which started on August 31, is located on a fissure at Holuhraun, an ice-free lava field north of Bardarbunga. Magma has been propagating from underneath the volcano, towards the eruption, causing subsidence and strong earthquakes in the floor of the Bardarbunga caldera.

The subsidence observed since last week is now up to about 20 metres, says Magnus Tumi Gudmundsson, professor of geophysics at the University of Iceland´s Institute of Earth Sciences.

He notes three possible scenarios regarding Bardarbunga. Firstly that the seismic activity, and the Holuhraun eruption, dies down slowly. A second scenario would see the subsidence continue, as well as the Holuhraun eruption, or even another eruption starting nearby.

"But the third scenario is that the subsidence in the floor of the caldera causes an eruption within Bardarbunga. Such an eruption could melt a large volume of glacial ice, and could end up as a powerful explosive eruption, with ashfall," says Dr. Gudmundsson. "The meltwater would perhaps not be released immediately, due to the contour of the caldera, but eventually it would come out as a powerful flood. Obviously, we are worried about this possibility."

This scenario is regarded as very serious, not least because of the potential for a flood, which could cause extensive damage, says the director of the Civil Protection Agency in Iceland, Vidir Reynisson. "We are gravely concerned about this scenario. If we study the history of the Bardarbunga volcano, we see large and powerful eruptions in or near the caldera; we are bound to take this very seriously, especially after the subsidence was observed."

Tomorrow, Reynisson and his colleagues at the Civil Protection Agency will brief the Prime Minister of Iceland, Sigmundur David Gunnlaugsson, on the situation at Bardarbunga. Today, Reynisson met with the National Power Company, (Landsvirkjun), to discuss the potential consequences of a major flood from Bardarbunga threatening hydropower plants to the west of Vatnajokull glacier, which covers the volcano.

"As soon as the subsidence started in Bardarbunga, the National Power Company acted to minimize the risk of damage due to a potential flood," says Reynisson. "Should an eruption occur in Bardarbunga, it would obviously be of vital importance to pinpoint the location of the eruption inside the caldera, so we could predict the direction of a possible flood. Our reaction would then depend on that information." The caldera itself covers about 80 square kilometres, and lies under a 700-800 metre thick ice cap.
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