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Originally posted by TrueAmerican
There is just no way of knowing until it happens.
What sort of damages will occur when this thing goes? How long will the ash persist? Effects of the flooding?
Again, totally depends on the size of the eruption. Locally, people seem relatively prepared. For one thing, they have avoided population centers around the immediate vicinity of Katla, so there are few people who would die there from the immediate effects, unless the eruption was so big the pyroclastic flows and debris reached beyond the radius expected.
Iceland was buried under ice in the last Ice Age and all eruptions were subglacial. Remnants of the ice caps remain and Iceland continues to have numerous subglacial eruptions. Of the world's known subglacial eruptions, 83% are in Iceland. The most recent eruption, at Grimsvotn, is an example. Subglacial eruptions produce a special type of volcano, called a table mountain or a moberg mountain. Great volumes of meltwater, generated by subglacial eruptions, can burst out from beneath glaciers to produce enormous floods called jokulhlaup. The discharge can be as much as 20 times greater than the flow rate of the Amazon River.
The 1783 eruption at Laki was the largest single historic eruption of basaltic lava (12 cubic km). Recent eruptions include the 1974-1984 eruption at Krafla, a brief eruption at Hekla in 1991 and again on February 26 2000 and three eruptions at Grimsvotn, in 1996, 1998 and 2004.
In Katla´s last eruption in 1918 icebergs the size of houses were seen floating out to sea. More recently in 1955 and 1979 there have been floods though no eruption that you could see.
So PuterMan, would you say these are occurring in the typical locations that indicate that they are part of this summer/winter "refreeze" you mention? Or are they occurring in new locations?
Between late 2000 and early 2005 there was a moderate increase in seismicity rate beneath Katla caldera, and a much greater increase in seismicity rate in the Goðabunga area, on the west flank of Katla. The increase in seismicity was approximately coincident with upwards and radially outwards movement of two campaign GPS stations north of Katla caldera [7]. This motion has since ceased, but two continuous GPS sites on the southern flank have been trending upwards and south-southwest, after subtraction of plate-spreading motion, since installation in 2000 [8], and this motion continues to the present.
We find that there is no significant systematic motion of the flanks of Katla from 1995 to 1998 and from 2000 to 2006, other than that expected from thinning of Vatnajökull and Mýrdalsjökull ice caps. We conclude that increased seismicity in the region of Goðbunga was not accompanied by significant deformation. We also
detect local variations in velocities that may be due to landsliding.
ABSTRACT. The Katla volcano, overlain by the Myrdalsjokull glacier, is one of the most active and hazardous volcanoes in Iceland. Earthquakes show anomalous magnitude-frequency behaviour and mainly occur in two distinct areas: within the oval caldera and around Goðabunga, a bulge on its western flank. The seismicity differs between the areas; earthquakes in Goðabunga are low frequency and shallow whereas those beneath the caldera occur at greater depths and are volcano-tectonic. The seismicity shows seasonal variations but the rates peak at different times in the two areas. A snow budget model, which gives an estimate of the glacial loading, shows good correlation with seismic activity on an annual scale. Data recorded by the permanent network South Iceland Lowland (SIL), as well as by a temporary network, are used to invert for a 3D seismic velocity model underneath Eyjafjallajokull, Goðabunga and the Katla caldera. The tomography resolves a 15 km wide, aseismic, high-velocity structure at a depth of more than 4 km between the Eyjafjallajokull volcano in the west and the Katla volcano in the east. Anomalously low velocities are observed beneath the Katla caldera, which is interpreted as being a significantly fractured area of anomalously high temperature.
consistent with the visual observation that the Goðabunga seismicity has a maximum in October and the snow budget a minimum in September
Originally posted by TrueAmerican
Originally posted by Spacedman13
Katla´s crater has hardly had any quakes.
Well, just today look:
Quakes inside the rim, and more on the edges!
In 1918 they didn't have the kind of monitoring they have now... So once it does blow, it will give science valuable information for future generations.
Some volcanoes may be so closely spaced that they are coupled; activity in one system has a profound influence on the other. One such pair includes the Katla and Eyjafjallajökull volcanoes
Mr Kjartansson says that the flooding is also considered to have brought a 2,000-ton rock from the volcano to the black volcanic desert of Mýrdalssandur, while also extending the beach by a factor of 2km within the first 24 hours of the 1918 eruption.
Originally posted by TrueAmerican
PuterMan, quick question for you:
How would you characterize Iceland's warning capabilities before Eyja erupted? In other words, did eruption occur as expected, or did it come as a surprise?
In regards to the high velocity structure found (tomography) between the two volcanoes, Eyja and Katla, would that not indicate a high level of independence?
Originally posted by PuterMan
reply to post by TrueAmerican
Sorry forgot to answer the first part. No, all I recall is that the geologists were talking about it, but i don't think any warnings were given.edit on 5/10/2010 by PuterMan because: (no reason given)