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.
The caldera of the volcano has a diameter of 10 km (6 mi) and is covered with 200-700 metres (660-2,300 ft) of ice. The volcano normally erupts every 40–80 years. The flood discharge at the peak of an eruption in 1755 has been estimated at 200,000–400,000 m³/s (7.1-14.1 million cu ft/sec), comparable to the combined average discharge of the Amazon, Mississippi, Nile, and Yangtze rivers (about 266,000 m³/s (9.4 million cu ft/sec)).
Katla has been showing signs of unrest since 1999, and geologists have concerns that it might erupt in the near future.[9] Particularly, monitoring has been intensified following the March 2010 eruptions of a smaller neighbouring volcano - Guðnasteinn - beneath the Eyjafjallajökull glacier.[10] The eruption of this nearby long-dormant volcano in March and April 2010 prompted fears among some geophysicists that it might trigger an eruption at the larger and more dangerous Katla.[11][12][13] In the past 1,000 years, all three known eruptions of Eyjafjallajökull have triggered subsequent Katla eruptions.[14] Following the 2010 Eyjafjallajökull eruptions, on 20 April 2010 Icelandic President Ólafur Grímsson said "the time for Katla to erupt is coming close ... we [Iceland] have prepared ... it is high time for European governments and airline authorities all over Europe and the world to start planning for the eventual Katla eruption".[15]
Originally posted by Anmarie96
There is a swarm ongoing at Bardarbunga - but it doesn't show on Their map?
It's as if that whole country is constantly shaking
Since 1999, that is considerable uplift at a station positioned right on the volcano itself. Note that is the up/down axis. The other axes are here, but they don't matter as much:
Glaciers in Iceland began retreating around 1890, and since then the Vatnajokull ice cap has lost over 400 km3 of ice. The associated unloading of the crust induces a glacio-isostatic response. From 1996 to 2004 a GPS network was measured around the southern edge of Vatnajokull. These measurements, together with more extended time series at several other GPS sites, indicate vertical velocities around the ice cap ranging from 9 to 25 mm/yr
There is a swarm ongoing at Bardarbunga - but it doesn't show on Their map? Why?
Originally posted by PuterMan
It's as if that whole country is constantly shaking
@TrueAmerican. Maybe it is! After all it is sat on a mantle plume larger than Yellowstone if you believe the tomography at either place.
[atsimg]http://files.abovetopsecret.com/images/member/137eefaa9620.jpg[/atsimg]
Mm, sort of puts that small time slice in it's place I think despite the fact that it is a little out of date.
This one is not out of date
All in all I personally don't feel there is much to be worrying about at present.
Incidentally the Eyja/Katla connection is a fact however to some degree the connection as far as Katla going after Eyja is anecdotal since Katla erupts far more often that Eyja and therefore there is a good chance of this occurring.
Originally posted by TrueAmerican
And so you are suggesting that's the reason these background levels are so high at BORG? I would assume that's what you mean...
Tell me, do YOU believe the (seismic) tomography?
Yeah, a whole month out of date...You have any recent info? Everything here in this thread is as of today.
Yeah, but that's Eyja, I am concentrating on Katla.
And so now I have another question...What about gas emissions? I cannot find anything on that for Katla, and I don't see anything at the Iceland Met Office referring to them...
We've got quakes on the volcano. And as far as uplift, maybe you ought to take a look at that video in the OP. The subsidence (depressions) in the ice can actually be because the heat underneath is melting the ice cap. How can they even be sure that there ISN'T uplift of the actual dome underneath 600 to 2000 feet of ice?
Oh? I though they erupted roughly in the same amount, and back to back? Hmm, got any info on that?
Originally posted by PuterMan
By the way Katla has a magma chamber of about 21 cu km if you are interested. That is a VEI 5 if my memory serves me right.
Originally posted by PuterMan
By the way Katla has a magma chamber of about 21 cu km if you are interested. That is a VEI 5 if my memory serves me right.
Originally posted by Tarrok
I just checked Wiki, it's a VEI 6.
What sort of damages will occur when this thing goes? How long will the ash persist? Effects of the flooding?
Originally posted by Anmarie96
In addition, there is no instrument on Katla that they are sharing the information.
From here you can view tremor plots from all our seismic stations.
Originally posted by Anmarie96
Umm - Godabunga is off to the northwest side of Katla in between Eyjaxyz and Katla. This area IMO has been shaking much more than is usual and while the season is changing and the ice (dreaded ice) is going through changes, I think there is more to it than that. LOL love the way it's always the fault of the Ice
The Katla volcano is covered by the Mýrdalsjökull ice cap and is currently one of the most active volcanoes in Iceland. It has erupted twenty times the past 1,100 years. The neighbouring volcano Eyjafjallajökull has erupted twice, simultaneously with Katla. As glaciers cover both volcanoes, their eruptions are phreato-magmatic by nature. The volcanoes are located directly south of where surface expressions of the rift cease. Seismically, Katla is one of the most active volcanoes in Iceland, showing an annual cycle in activity, observed from at least 1960 and less pronounced since 2004. From 1999 to late 2004, GPS measurements revealed steady inflation of the volcano, showing uplift and outward horizontal displacement....
The earthquakes under Goðabunga show a clear seasonal correlation with a distinct activity during the autumn. This pattern changed in 2002 to more continuous activity. The earthquakes in the caldera have a swarm character, and the largest earthquakes occur there.
In recent years Katla and Grı´msvo¨ tn have shown the highest inflation rates with ca. 3 cm/a. and tilt data from Hekla suggest that magma accumulation is taking place. At Katla, continued uplift coincides with elevated seismicity. If uplift and internal pressure build-up continues at these volcanoes, eruptive activity is a likely consequence within several years.