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Originally posted by kissitgoodbye
reply to post by Moshpet
Question: Today is June 22, 2011. I looked at the seismographs for Yellowstone. How would you know if the volcano was in preeruption mode? From what I have read there would be small quakes in the area first. That's happened already. Now we have YJC monitor going nuts and YNR in the area already off line. It has been for a while. YMR is showing significant activity too. Even if you go back to the first part of June and look at the seismo's going forward until now. It is of concern to me, but I'm not an expert. Just been following the pattern developing.
I know you were right about how earthquakes in other parts of the world have an effect here too. That is part of my concern as well.
I saw what happened at Yellowstone on the seismo's when the Japanese quake occurred. Now the Chile quake the other day, and waves going straight up to Yellowstone. How can you tell if this is crap instead of accurately warning of an impending problem? Thanks for your input.
I saw what happened at Yellowstone on the seismo's when the Japanese quake occurred. Now the Chile quake the other day, and waves going straight up to Yellowstone.
Originally posted by asmall89
Uh so is this not normal then? I go to college right next to the thing! Now I really don't want to go back there after break. From somewhere I heard the date was 2010 or 2012, too bad I can't recall the source... Thats scary.
Originally posted by Springheel Jack
I think that some here are giving in to the fear monster a bit. Yes Yellowstone is a supervolcano and yes it is seismically active, and yes it could erupt but just a few minutes of reading can help us understand that there are many telltales leading up to an eruption.....
General principles of volcano seismology
Seismic activity (earthquakes and tremors) always occurs as volcanoes awaken and prepare to erupt and are a very important link to eruptions.........
Be prepared. Make sure if you live near that beast you have a plan, but don't go running around saying the sky is falling yet. I would bet the USGS keeps a close tabs on it.
Overall, geophysical and geochemical evidence points strongly towards the presence of a large thermal anomaly in the shallow- to mid-crust. Given the size of the caldera and the implied depths, it is reasonable to infer that at least 15 000 km 3 of crystal-melt mush are located beneath the Yellowstone caldera, at depths from Figure 2. Diagram illustrating seismic-wave-velocity anomalies in the shallow crust beneath Yellowstone as viewed from the southwest (adapted from Husen et al. 2004a). The orange volume outlines the anomaly attributed to partially molten rock extending above the main magma chamber (and beneath the surface expressions of the Sour Creek and Mallard Lake resurgent domes).
The red volume is an anomaly with properties suggesting gas-filled fractured rock. The green dots are hypocentres from the 1985 earthquake swarm. The arrows are postulated trends of hydrothermal fluid flow from the magma body to the inferred gas-filled body as discussed by Waite & Smith (2002) and Husen et al. (2004a). Though the tomographic imaging of Husen et al. (2004a) did not extend beneath 12 km depths, other workers have inferred partially molten crustal magma chambers extending to ca 20 km beneath the caldera (Iyer et al. 1981; Lehman et al. 1982). Monitoring super-volcanoes 2061 Phil. Trans. R. Soc. A (2006)ca 8 to 18 km.
If melt fractions are 0.1–0.15, then sufficient melt exists to form the mass for a super-eruption—if it can be extracted and accumulated into an eruptible volume. Most geophysical images have insufficient resolution to define volumes less than ca 10 km on a side. It is fully plausible that volumes with high melt fractions (more than 0.6) exist within dikes and sills within the greater magma chamber, and could erupt as moderate-volume (less than 100 km 3 ) lavas or pyroclastic flows. Current evidence suggests, however, that the gravity and seismic anomalies are not sufficiently large to allow for a larger, highly molten (and thereby eruptible) volume of magma beneath Yellowstone at this time.
. Yellowstone: current activity Despite Yellowstone’s long period of volcanic dormancy, now over 70 000 years, the caldera continues to be an active and dynamic environment, with thousands of earthquakes, active ground deformation and considerable heat and mass flux. The monitoring system of the Yellowstone Volcano Observatory (volcanoes.usgs. gov/yvo) is designed to listen to these signals, to see how they relate to each other, and to provide adequate characterization of background activity. Only by cataloguing the range of normal activity can we start to decipher the signals emanating from caldera systems headed towards eruption. Here, we now address the kinds of Earth signals documented over the past 50 years
1- there is a supporting theory that states that larger quakes along one fault line can trigger tremors and smaller quakes as far as 2000 km away according to a study done by geologists (USGS, sorry can't find the link)
3.0 Non-technical Summary
We hypothesize that large remote earthquakes trigger earthquakes in southern California. We assume the same mechanism of triggering applies to both local and remote mainshocks. We quantitatively estimate a triggering (non-triggering) threshold using local mainshocks, and find triggering events generally reach higher spectral amplitudes in the range of 0.1-10 Hz. Assessing ~40 remote mainshocks (M>7.0) we find no obvious signature of remote triggering. Comparing spectral characteristics, we conclude: (1) triggering is a complex combination of amplitude and frequency; and/or (2) there is a time-to-failure component we have not accounted for; and/or (3) remote and local events have different triggering mechanisms.
and could erupt as moderate-volume (less than 100 km3)
The second phase is estimated to be a VEI 4 eruption
YELLOWSTONE VOLCANO OBSERVATORY MONTHLY UPDATE
Friday, July 1, 2011 11:31 AM MDT (Friday, July 1, 2011 17:31 UTC)
YELLOWSTONE VOLCANO (CAVW #1205-01-)
44°25'48" N 110°40'12" W, Summit Elevation 9203 ft (2805 m)
Current Volcano Alert Level: NORMAL
Current Aviation Color Code: GREEN
During the month of June 2011, 64 earthquakes were located in the Yellowstone National Park region. The largest was a magnitude 2.3 event on June 19 at 3:14 AM MDT, located about 10 miles south southeast of West Yellowstone, MT. No swarms were recorded in June.
Earthquake activity continues at relatively low background levels. For a map of recent earthquakes, please see:
www.seis.utah.edu...
Ground Deformation Summary: The period of caldera uplift that began in 2004 ended over one year ago. Since then, the caldera has been subsiding, though seasonal deformation from ground water changes may temporarily mask the trend. Please see: www.uusatrg.utah.edu... for a map of GPS stations in the Yellowstone vicinity. For a graph of daily GPS positions at White Lake, within the Yellowstone caldera, please see: pboweb.unavco.org...�eries=raw.