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The Mw 8.8 Maule earthquake on 27 February 2010 triggered hundreds of local volcano-tectonic events at Uturuncu. High-pass filtering of the long period surface waves reveals that the first triggered events occurred with the onset of the Rayleigh (R1) and Love (G1) waves. Activity gradually declined following the passage of the R1 and G1 waves, however rates of triggered events increased again with the passage of the R2/R3 and G2/G3 surface waves. To the best of our knowledge, this is the first time such triggering has been observed for multiple surface wave trains from the same large earthquake. All the observations together suggest metastable conditions in the shallow summit region of Uturuncu volcano.
We find that the 270 ky dormant Uturuncu Volcano in SW Bolivia exhibits relatively high rates of shallow, volcano-tectonic seismicity that is dominated by swarm-like activity. We also document that the 27 February 2010 Mw 8.8 Maule, Chile earthquake triggered an exceptionally high rate of seismicity in the seconds to days following the main event. Although dormant, Uturuncu is currently being studied due to its large-scale deformation rate of 1-2 cm/yr uplift as revealed by InSAR. As part of the NASA-funded Andivolc project to investigate seismicity of volcanoes in the central Andes, a seismic network of 15 stations (9 Mark Products L22 short period and 6 Guralp CMG40T intermediate period sensors) with an average spacing of about 10 km was installed at Uturuncu from April 2009 to April 2010. Volcano-tectonic earthquakes occur at an average rate of about 3-4 per day, and swarms of 5-60 events within a span of minutes to hours occur a few times per month. Most of these earthquakes are located close to the summit at depths near and above sea level. The largest swarm occurred on 28 September 2009 and consisted of 60 locatable events over a time span of 28 hours. The locations of volcano-tectonic earthquakes at Uturuncu are oriented in a NW-SE trend, which matches the dominant orientation of regional faults and suggests a relationship between the fault system at Uturuncu and the regional tectonics of the area; a NW-SE trending fault beneath Uturuncu may serve to localize stresses that are accumulating over the broad area of uplift. Based on automated locations, the maximum local magnitude of these events is approximately M = 4 and the average magnitude is approximately M = 2. An initial estimate of the b-value is about b = 1.2. The Mw 8.8 Maule earthquake on 27 February 2010 triggered hundreds of local volcano-tectonic events at Uturuncu. High-pass filtering of the long period surface waves reveals that the first triggered events occurred with the onset of the Rayleigh (R1) and Love (G1) waves. Activity gradually declined following the passage of the R1 and G1 waves, however rates of triggered events increased again with the passage of the R2/R3 and G2/G3 surface waves. To the best of our knowledge, this is the first time such triggering has been observed for multiple surface wave trains from the same large earthquake. All the observations together suggest metastable conditions in the shallow summit region of Uturuncu volcano.
reply to post by TrueAmerican
Heck, that volcanic system deep underground may have everything to do with all the quakes in the area. They say anything that happens within a 200 km mile radius of Yellowstone is likely in some way connected to the park. Some say 500 km radius.
Uturuncu is surrounded by one of the most dense concentrations of supervolcanoes on the planet, all of which fell silent some 1 million years ago.
(Oregon State University Professor) De Silva said it appears that local volcanoes hoard magma for about 300,000 years before they blow — and Uturuncu last erupted about 300,000 years ago.
"So that's why it's important to know how long this has been going on," he said.
Originally posted by nineix
Extremely fascinating though. It's amazing how fast that thing is growing. Wow!
reply to post by JustMike
Okay, this could take decades or even centuries to lead to anything drastic -- if it does even then. Not hitting any panic buttons yet! But we'd be wise to keep track of it and I for one thank TrueAmerican for bringing this to our notice.
reply to post by TrueAmerican
Yeah, no doubt. I just ran some numbers. If that inflation rate holds at its present rate for just the next three months, that chamber will have increased in size by a whopping 259,200 CUBIC METERS ! And in a year, by over 1,036,800 CUBIC METERS. But I digress. The documented triggering aspect of this from a large quake nearby is truly unnerving. I think it's safe to say that as long as that thing is growing, the more unstable it becomes. The more pressure is put on the capping rock, the more the risk of water entering the chamber (boom), and the closer it is to erupting. We can only hope that it behaves like many other volcanoes and starts into a period of deflation. SOON. !
at a rate of a cubic meter of magma PER SECOND
reply to post by CosmicEgg
I was laughed out of my science courses for asking this question back in the day. Glad to see that science finally made the connection. Sure takes time though! You'd think it would be a fairly straightforward connection, eh? O_O
Originally posted by TrueAmerican
reply to post by MamaJ
I tell ya what. I confess that I watch all this stuff going on ATS and elsewhere, and have never really felt that I needed to do the whole survival thing before, even in the face of riots, economic disaster, etc.
But this?
THIS could be the reason the elites are building bunkers. THE secret that is just now getting out. They tantalize us with movies about Yellowstone and Deep Impacts, while the whole time the real killer has been lurking and growing like a mega zit behind the scenes.
[/trip]*smacks meeself* - get that imagination back in the cage man. Ok, phew.... I'm back to now.
Originally posted by PuterMan
error. Back in a moedit on 22/10/2011 by PuterMan because: (no reason given)
Researchers realized about five years ago that the area below and around Uturuncu is steadily rising — blowing up like a giant balloon under a wide disc of land some 43 miles (70 kilometers) across. Satellite data revealed the region was inflating by 1 to 2 centimeters (less than an inch) per year and had been doing so for at least 20 years, when satellite observations began.
reply to post by JustMike
But here's the problem: so little is known about what happens with supervolcanoes as they enter their eruptive state. There are theories, sure, but we've never actually seen one in modern times. Toba was the last "big one" and there is evidence that it came pretty close to wiping humans out altogether. (Some dispute the genetic arguments on that score, though.)