It looks like you're using an Ad Blocker.
Please white-list or disable AboveTopSecret.com in your ad-blocking tool.
Thank you.
Some features of ATS will be disabled while you continue to use an ad-blocker.
originally posted by: larapa
a reply to: aboutface
This is what happened last time Baroarbunga went off:
originally posted by: larapa
a reply to: aboutface
This is what happened last time Baroarbunga went off:
Overall assessment from the joint daily status report 240814 of the Icelandic Met Office and the University of Iceland, Institute of Earth Sciences:
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 colour-code from red to orange.
M5.7 - 116km SSE of Akureyri, Iceland 2014-08-26 01:26:08 UTC
Location 64.665°N 17.500°W depth=5.0km (3.1mi)
Nearby Cities
116km (72mi) SSE of Akureyri, Iceland
M5.7 ) ENE of Reykjavik, Iceland
221km (137mi) ENE of Kopavogur, Iceland
224km (139mi) ENE of Hafnarfjordur, Iceland
612km (380mi) WNW of Torshavn, Faroe Islands
At 16:19 UTC an earthquake of magnitude 5,1 occurred on the southern rim of the Bárðarbunga caldera. Events of similar magnitude have already occurred in recent days in the same area at 2-6 km depth. These events are considered to be linked to subsidence of the volcano due to volume changes in the magma reservoir underneath. Activity along the intrusion is continue's.
Iceland volcano: New quakes raise concern over large eruption
British and Icelandic scientists say that 50 million cubic metres of molten rock has moved in a 24 hour period.
If it continues to head north, it could link up with the Askja system and trigger a large eruption.
Scientists working in the area have said that they will be withdrawing from the exclusion zone on Wednesday after they have deployed some more instruments
Over the last 10 days, they have detected large numbers of earthquakes, which have been moving north over a distance of about 40km. They are caused as magma flows beneath the ground, cracking the rocks as it moves.
On Tuesday morning the Bardarbunga volcano was hit by a magnitude 5.7 earthquake, the largest since tremors began in the area last week.
About 350 million cubic metres of magma have moved in this period, which is about twice the amount of molten rock that was blasted into the air during Iceland's Eyjafjallajokull eruption in 2010.
Prof Simon Redfern, an earth scientist from the University of Cambridge, said: "It is a huge amount of magma, creating an enormous subterranean channel of molten rock."
He said that the dyke - the underground "plumbing system" that carries the molten rock - could join up with other underground fissures, creating a large network of magma
"But who knows, it may just stop. It is still at 5km-depth, and it is possible it could freeze there and not a lot more will happen. That is perfectly plausible."
Scientists from IES and IMO on a flight to Vatnajökull tonight discovered a row of 10-15 m deep cauldrons south of the Bárðarbunga caldera. They form a 6-4 km long line. The cauldrons have been formed as a result of melting, possibly a sub-glacial eruption, uncertain when.
Link
Geologists in Britain and Iceland have said 50 million cubic metres of molten rock has moved in a 24 hour period and it could reach Askja in just a few days.
We know there is a lot of molten rock sitting under the ground beneath Askja, which is a major volcanic system. If this molten rock hits that, we know it is likely to trigger it to erupt.
link
originally posted by: aboutface
a reply to: glend
What specifically do you mean by dyke in the context of a volcano? I'm feeling quite dense at the moment.