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emphasis mine
An emerging challenge in modern volcanology is the apparent contradiction between the perception that every volcano is unique, and classification systems based on commonalities among volcano morphology and eruptive style. On the one hand, detailed studies of individual volcanoes show that a single volcano often exhibits similar patterns of behavior over multiple eruptive episodes; this observation has led to the idea that each volcano has its own distinctive pattern of behavior (or “personality”). In contrast, volcano classification schemes define eruption “styles” referenced to “type” volcanoes (e.g., Plinian, Strombolian, Vulcanian); this approach implicitly assumes that common processes underpin volcanic activity and can be used to predict the nature, extent and ensuing hazards of individual volcanoes. Actual volcanic eruptions, however, often include multiple styles, and type volcanoes may experience atypical eruptions (e.g., violent explosive eruptions of Kilauea, Hawaii, Fiske et al., 2009). The volcanological community is thus left with a fundamental conundrum that pits the uniqueness of individual volcanic systems against generalization of common processes. Addressing this challenge represents a major challenge to volcano research.
To answer this question, it is important to assess the goals of volcano research. One goal is to improve the safety of communities that live close to active volcanoes. Here identifying one or more reliable precursors to an impending eruption [e.g., identification of tornillos at Galeras volcano, Columbia (Lourdes et al., 1997)] may not only be sufficient to meet that goal (that is, knowledge of the individual volcano may be enough), but may be the most appropriate and accurate approach. Individual volcano knowledge, in fact, underpins recent advances in developing effective strategies for volcano monitoring (Ewert et al., 2005; Miller and Jolly, 2014) and forecasting (Lindsay et al., 2010; Marzocchi and Bebbington, 2012; Bebbington, 2013) using statistical approaches such as risk trees and probabilistic models. A second goal is global, and focuses on acquisition of volcano parameters that can be used to identify regions of high volcanic hazard (and risk), and to place hazard assessments of specific volcanoes within a global context.
originally posted by: TrueAmerican
originally posted by: rickymouse
Are you saying the people living around there may be screwed?
No. I'll let the authorities determine that.
How is seismic data from one of those different than other seismic activity?
1) In that what little is seen of tornillos, they are almost always associated with fluid movement of some kind, and they only happen at select volcanoes. Apparently they happened at St. Helens and at Redoubt before eruptions.
2) Whereas both quakes and tremor can be associated with hydrothermal activity, or even gas activity, most of the time tornillos indicate magma movement (or at least so they think).
In studying some of these signatures more, like the ones from today, the apparent lack of energy in the 1 to 2 hz bands leads me to believe they are probably very shallow. In some of the other ones I sent to them, however, the exact opposite is true. The actual predominate frequency of them is exactly in the 1 to 2 hz bands, complicating this mystery. It could suggest two separate source mechanisms, if they are both tornillos in the first place. In those cases I think they are deeper. Much deeper. See the OP for the pics.
originally posted by: tsctsc
originally posted by: TrueAmerican
originally posted by: rickymouse
Are you saying the people living around there may be screwed?
No. I'll let the authorities determine that.
How is seismic data from one of those different than other seismic activity?
1) In that what little is seen of tornillos, they are almost always associated with fluid movement of some kind, and they only happen at select volcanoes. Apparently they happened at St. Helens and at Redoubt before eruptions.
2) Whereas both quakes and tremor can be associated with hydrothermal activity, or even gas activity, most of the time tornillos indicate magma movement (or at least so they think).
In studying some of these signatures more, like the ones from today, the apparent lack of energy in the 1 to 2 hz bands leads me to believe they are probably very shallow. In some of the other ones I sent to them, however, the exact opposite is true. The actual predominate frequency of them is exactly in the 1 to 2 hz bands, complicating this mystery. It could suggest two separate source mechanisms, if they are both tornillos in the first place. In those cases I think they are deeper. Much deeper. See the OP for the pics.
If you don't mind my (maybe very) silly question, however, not long ago there was a topic here saying about some sort of cannyon that cracked open in Wyoming (www.abovetopsecret.com...).
Now, this tornillos in Mt Rainier... considering that both States (WY and WA) are surrounding the Rocky Mountains (forgive me if I'm mistaken, geophysical maps is not exactly my strongest), wouldn't it be too much of a coincidence? Maybe there is some tectonic movement really taking place?
Also (and I don't want to be alarmist - please take into account my ignorance on the subject), if there's something going on up in northwestern US, could this cause or be a consequence of impact in southwestern US (read St. Andreas)?
As I keep reading ATS's topics (as well as other fora), time and time again recently people are writing about all sort of phenomena in that west "strip". Birds behaving strangely, dead fishes, insects plagues.... I dunno.
Maybe those are all unrelated... maybe not. Do you have any insight about it?
originally posted by: OneGoal
originally posted by: tsctsc
originally posted by: TrueAmerican
originally posted by: rickymouse
Are you saying the people living around there may be screwed?
No. I'll let the authorities determine that.
How is seismic data from one of those different than other seismic activity?
1) In that what little is seen of tornillos, they are almost always associated with fluid movement of some kind, and they only happen at select volcanoes. Apparently they happened at St. Helens and at Redoubt before eruptions.
2) Whereas both quakes and tremor can be associated with hydrothermal activity, or even gas activity, most of the time tornillos indicate magma movement (or at least so they think).
In studying some of these signatures more, like the ones from today, the apparent lack of energy in the 1 to 2 hz bands leads me to believe they are probably very shallow. In some of the other ones I sent to them, however, the exact opposite is true. The actual predominate frequency of them is exactly in the 1 to 2 hz bands, complicating this mystery. It could suggest two separate source mechanisms, if they are both tornillos in the first place. In those cases I think they are deeper. Much deeper. See the OP for the pics.
If you don't mind my (maybe very) silly question, however, not long ago there was a topic here saying about some sort of cannyon that cracked open in Wyoming (www.abovetopsecret.com...).
Now, this tornillos in Mt Rainier... considering that both States (WY and WA) are surrounding the Rocky Mountains (forgive me if I'm mistaken, geophysical maps is not exactly my strongest), wouldn't it be too much of a coincidence? Maybe there is some tectonic movement really taking place?
Also (and I don't want to be alarmist - please take into account my ignorance on the subject), if there's something going on up in northwestern US, could this cause or be a consequence of impact in southwestern US (read St. Andreas)?
As I keep reading ATS's topics (as well as other fora), time and time again recently people are writing about all sort of phenomena in that west "strip". Birds behaving strangely, dead fishes, insects plagues.... I dunno.
Maybe those are all unrelated... maybe not. Do you have any insight about it?
The san andreas and juan de fuca plate have corresponding boundaries. The juan de fuca is directly responsible for the cascadia region being volcanic.
There is a correlation between san andreas and the juan de fuca plates. Id imagine a large san andreas slip could lead to a juan de fuca slip at worst.