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The earthquake activity in Bárðarbunga volcano has been migrating to the north-east over the past 10 to 18 hours. The activity close to Dyngjuháls appears to be stable at that location for the moment. Earthquake activity in other parts of Bárðarbunga have quieted down for the moment, that might change without warning.
originally posted by: Aromaz
Actually I am surprised by the little interest from major news media ... and even here on ATS for this volcano.
Too many little things happened and blunted peoples thread sensors?
Goodness - this is potentially THE disaster of the century to date.
originally posted by: Aromaz
IF Bárðarbunga erups, and ash goes more than 8,000 meters high ...
this one could be a MAJOR catastrophe.
Not only for the immediate time - but for a long few years.
Not only for Iceland and Europe but for all of the Northern Hemisphere.
Going back to what I stated about Nabro in 2011 that will affect the NH weather systems due to Sulphur ... and proved correct.
This Bárðarbunga is much worse.
Potentially it looks like it might be a big eruption.
In 4 days the quake depth rose form 15 km to 10 km or less.
4.5 quake yesterday and then a long series of somewhat strange harmonic .... these are usually visible recordings during an eruption.
This volcano has a history of serious poison gas.
In particular it emits very high levels of Sulphur and the highest known Hydrogen Fluoride content.
should that go high it will cool the Northern Hemisphere down by a few degrees Celsius.
While the northern cluster close to Kistufell has calmed down significantly following the M4.5 earthquake on early Monday morning, event rates in the eastern cluster are still high. Similar to recent days, two pulses of comparably strong seismic activity have been measured between 04:00 and 08:00 this morning, as well as 16:00 and 18:30 in the afternoon. The cluster east of Bárðarbunga continued to slowly migrate northeastwards today. Events are still located at around 5-12 km depths, no signs of upwards migration has been seen so far.