The clock is ticking in Sumatra, page 3
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reply posted on 14-4-2005 @ 12:24 AM by Indy
Here you go...

www.indonesia-relief.org...

"Jakarta, Detikcom - On Wednesday, Indonesia's Vice President Jusuf Kalla asked people living in area near of mount of Anak Krakatau (Child of Krakatoa) and Tangkuban Perahu to prepare from being evacuated. The VP announcement released as the danger level has been raised to level III on both volcanoes. "

While at some point before modern history things like this may have happened we must also wonder what else happened at this time. How far did the problem go? What is being observed now is unprecidented in modern times.



reply posted on 14-4-2005 @ 12:49 PM by Nygdan
Originally posted by Indy
Nothing weird is happening? Two quakes of 8.7+ in the same region only 3 months apart. 242 quakes of 4+ in Northern Sumatra in 30 days which is better than 1/3rd of the global quakes over 4.0 and you think there is nothing weird.

Indeed, its not weird.

Large quakes are running at about double what is normal but you think there is nothing weird?

How do you figure its double? The tightest resolution for earthquake activity on a regional scale is probably a year. This has been an average year.

. There has been a report of activity being triggered in Toba Lake by one of the quakes and nothing weird is happening.

Again, indeed, nothing weird. Earthquakes and volcanos are not weird.

Its entirely possible, tho not certain, that if humans had a clearer understanding of the system (supposing there is one) that they'd be able to say that these earthquakes should precede some volcanic activity.That, in itself, wouldn't be weird.

When Mt. St. Helens erupted it was preceded by small earthquakes.

However, there are earthquakes in that region because of intersecting tectnoic plate margins. So the analogy to small earthquakes that precede volcanic eruptions is not a good one.

Th best indicator that there might be some volcanic activity in the region, is, well, some of the volcanic activity that is starting.

But the big quakes have nothing to do with anything, certainly not systematically. Again, look at the information, it shows that there is a heck of a lot more tectonic activity all over the globe than people realize. Everyone is scarred because of the tsunami. Fear, however, is not a useful emotion in this case, and its obscuring any estimations of what is and what is not going on there.


reply posted on 14-4-2005 @ 02:19 PM by Ulvetann
Turkish Press

I found this as highly relevant to my posting in the Volcano Watch 2005 Section.

I think Indy is covering this very good!



reply posted on 14-4-2005 @ 05:53 PM by specialasianX
Of course in earths lifespan things like this happen... as we stated Krakatoa already has had two huge eruptions... Toba erupted 74000 years ago last (i'm not sure how regularly Toba erupts), and it was a HUGE eruption. Its one of these 'supervolcanos' that seem to be getting alot of attenttion these days... while i concede this Sumatra activiy is like to die down and come to nothing, as these things often do, the fact that a supervolcano is inevitably going to erupt at some point is daunting.

Also on the note that these quakes dont indicate any danger... i feel that is not neccesarly true. Prior ti Krakatoas 1883 eruption, for around three months, there was alot of seismic activity... Earthquakes, minor eruptions of the island etc etc... now while i'm confident Krakatoa wont erupt as it did in 1883 for a long time (the pressure hasnt built up to those levels as yet) I'm concerned that another volcano on the fault may be building that pressure. As the Indo-Australia palte subducts under the burmese (?) plate it takes with it, with each earthquake, and substantial amount of water... this water gets caught in subterranean magma chanbers and turns into steam... this steam builds up in pressure untill it is sufficiently vented... usually vias volcanic eruption. Now if one of these chamber has been building up with steam (and of course magma) for several centuries (or millenia), when it does vent it all out, it is likely to be in the form of a large explosion... this is exactly what hapened with Krakatoa 122 years ago... Also the Archipelago that is indonesia is no stranger to these large eruptions ans the whole country is effectively on a fault line...

This wont be 'the end of the world' as stated, our race will die out or move on before the end comes... but a large eruption of Toba could result in climate changing events... keep in mind the last eruption caused a 1000 year ice age... better to keep my eyes out for these things and be 'paranoid' than ignore the signs and be suprised... not that we can really do anything about it.


reply posted on 14-4-2005 @ 08:23 PM by silentlonewolf
I'm not sure about a supervolcano errupting but I would't be surprised to see a erruption similar to Mount Pinatubo back in 1991. (using this one just because it's a well known volcanic erruption.) Though this means almost nothing but here is the quake information preceeding pinatubo and a graph for Mt. St. Helens. Similar volacoes to what is in Indonesia i believe.


Numerous small earthquakes of the type that record fracturing of brittle rock (fig. 11A) continued through May. The earthquakes were generally too small to be felt, except very locally. For 1,800 earthquakes located between May 7 and June 1, magnitudes were less than 2.5. These earthquakes were strongly clustered in a zone between 2 and 6 km deep, located about 5 km north-northwest of the volcano's summit (fig. 12). Possibly, they recorded adjustments of the earth's crust to stresses
generated by growth or pressurization of a shallow body of magma.

USGS on Mount Pinatubo

Mt. St. Helens Seismicity graph

Notice the depth of the quakes. With the Mt. St. Helens Graph almost all are smaller than 10km depth.The depths of the quakes in indonesia are always around 20 Km or more. The seismology equipment weren't even used on Mt. St. Helens until just recently before the 1980 erruption.
Talang has shown some small shallow earthquakes, so if anything an erruption with some pyroclastics is about all I really fathom though.

Also, it's not so much the lava that gets you. It's the pyroclastic flows and subsiquent mudslides from one of those erruptions.
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