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Originally posted by PuterMan
reply to post by alysha.angel
Excellent, but my Norwegian isa little rustynon-existent so here is the link via Google language tools. Phew that's better!
[edit on 27/7/2010 by PuterMan]
The most recent eruptive phase of the volcano began on May 2, 2008, and is ongoing. According to the Global Volcanism Program, radiocarbon dating of older tephra from the volcano suggests that its last previous eruption was in 7420 BC ± 75 years.
Originally posted by PuterMan
reply to post by muzzy
I remember back in my school days seeing the pictures of the pink and white terraces that were destroyed in the last eruption (just before I was born ) but the mountain is not marked on the Smithsonian Volcano KMZ for Google! I wonder why?
They seem to miss a few - 2 in Iceland that I know of. I am steadily making a collection!
EVENTS LEADING TO AN ERUPTION The course of events likely to precede the next eruption at Okataina depends largely on whether the eruption is of basaltic or rhyolitic type. If the next eruption is basaltic it will probably occur with only a short period of seismicity, detected over a few days, or at most weeks, before the eruption. (The 1886 AD Tarawera eruption was preceded by no more than 1 hour of felt earthquakes!) This is because a basaltic eruption will probably involve a relatively small volume (» 1 km3) of low-viscosity magma which will rapidly fracture its way up through the earth’s crust from a depth of about 15 km. It will be difficult to distinguish the seismicity associated with this fracturing from the frequent non-volcanic earthquake swarms which now occur without associated eruptions, about once per year in the Okataina Centre. Deformation of the ground surface above the earthquake locations will probably precede and would help identify an impending eruption, if the deformation occurs within previously surveyed networks, such as those installed at Tarawera-Rotomahana, or near lakes used as tilt-level indicators, so that it can be instrumentally measured (see Figure 12). Ground deformation occurring elsewhere may not be detectable until becoming visible to the naked eye, probably immediately prior to the eruption. The short duration anticipated for precursory seismicity and ground deformation suggests that a basaltic eruption may not be usefully predicted. The eruption may occur before it could be confidently recognised as definitely impending.