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Our estimates suggest that the Yellowstone crustal magma reservoir contains partially molten material (5–15 % partial melt) that is considered a working model for the source of the caldera-forming dominantly rhyolitic eruptions of Yellowstone and the bimodal basaltic-rhyolitic volcanism of the Snake River Plain volcanic field.
...
We specifically note that assessments of Yellowstone volcanohazard [Christiansen et al., 2007] will not appreciably change with our new findings because the Yellowstone Late Quaternary volcanic history has been well defined in terms of ages, sizes, and frequency of eruptions that capture the record of the entire large magma body imaged here.
We estimate the reservoir contains considerable quantities of melt, >1000 km3, at melt fractions as high as ∼27%.
originally posted by: Realtruth
a reply to: SituationNAFU
If that area starts to Rock n Roll, a bunker is the last place to be.
Mother-Earth can humble even the toughest, and make the most unaware people, wake the heck up fast.
Another concern is that Glacier Peak has only one seismometer. The earthquake detectors pick up on swarms of tiny earthquakes that can indicate magma is moving toward the surface and lead to an eruption.
originally posted by: Alien Abduct
originally posted by: Navieko
a reply to: SituationNAFU
Yeah you're right, they've just done a revised threat level assessment which is based on the projected threat if a volcano erupts. What baffles me is how they considered Yellow Stone to only be a 'moderate' level threat prior to this assessment, and still only a 'high' level threat now - considering they have a 'very high' threat level. I would have thought Yellow Stone would top the list.
I was just thinking the same thing. I was thinking just the two facts; that Yellowstone is active, and that Yellowstone is a super volcano, should give Yellowstone a very high threat level.
originally posted by: MteWamp
From what I understand about Yellowstone, and I say this as a "Layman", at least as far as geology is concerned, if she were to blow, it's pretty much game over.
originally posted by: Flavian
originally posted by: Alien Abduct
originally posted by: Navieko
a reply to: SituationNAFU
Yeah you're right, they've just done a revised threat level assessment which is based on the projected threat if a volcano erupts. What baffles me is how they considered Yellow Stone to only be a 'moderate' level threat prior to this assessment, and still only a 'high' level threat now - considering they have a 'very high' threat level. I would have thought Yellow Stone would top the list.
I was just thinking the same thing. I was thinking just the two facts; that Yellowstone is active, and that Yellowstone is a super volcano, should give Yellowstone a very high threat level.
Super Volcanoes very rarely actually have super volcanic eruptions. Most activity is much smaller scale. And of your super volcanoes, Long Valley shows far more indications of a larger scale eruption (even then not necessarily a super eruption).
In short, this list makes perfect sense as it simply reflects the threat posed by volcanoes to the US populace / infrastructure.
In reality, Mount Rainier is far more threatening than Yellowstone in terms of death and damage UNLESS Yellowstone goes all super eruptive.
originally posted by: Flavian
originally posted by: MteWamp
From what I understand about Yellowstone, and I say this as a "Layman", at least as far as geology is concerned, if she were to blow, it's pretty much game over.
Not necessarily. Look at Mount Tambora in 1815 - a VEI level of 7. In fact, the only confirmed VEI level 7 since Lake Taupo roughly 180 AD. Super Eruptions are VEI 8 but these 2 are the closest we have to that in all recorded human history.
Looking at Tambora, what happened? Well all vegetation on the island was obliterated. Trees were uprooted and mixed with ash, forming rafts up to 5 km across. Ships encountered these over 2000 miles away. It produced a 4m high tsunami (way smaller than, for example, the Japan earthquake). Roughly 48'000 died on Sumbawa (where Tambora is located) but many of these were also due to disease and starvation, rather than simply from the blast. Bear in mind that Sumbawa is an island - an explosion that large, if you believe your Hollywood style doom porn, would have obliterated everyone on the island - but it didn't.
challenge accepted lol
originally posted by: SituationNAFU
a reply to: fightzone58
Try surfing on a lava wave in a firenado.
watch a documentary about mt st helens. its hard to hide a mountain growing 5 feet a day for a month and a half. we would all know
originally posted by: shawmanfromny
The real "doom porn" is the fact that the general public won't be notified in advance when Yellowstone is about to pop it's cork. The government knows all too well that any warning would incite a public panic that couldn't be controlled. The wealthy elite and a few politicians will all be shuttled to their underground luxury bunkers, while utter chaos erupts above ground. Things should get a tad dicey.
When erupting, all volcanoes pose a degree of risk to people and infrastructure, however, the risks are not equivalent from one volcano to another because of differences in eruptive style and geographic location. Assessing the relative threats posed by U.S. volcanoes identifies which volcanoes warrant the greatest risk-mitigation efforts by the U.S. Geological Survey and its partners. This update of the volcano threat assessment of Ewert and others (2005) considers new research in order to determine which volcanic systems should be added or removed from the list of potentially active volcanoes, updates the scoring of active volcanoes, and updates the 24-factor hazard and exposure matrix used to create the threat ranking. The threat assessment places volcanoes into five threat categories: very low, low, moderate, high, and very high. Within all five threat categories there are changes in relative rankings of volcanoes, and in a few cases, volcanoes moved between categories owing to changes in our understanding of their hazard, unrest, and exposure factors. Scorings of hazard factors were updated for some volcanoes where new research has identified Holocene eruptive activity or clarified our understanding of Holocene eruptive history and the occurrence of particular hazards such as tephra fall or pyroclastic density currents. The most numerous scoring changes made in the threat matrix since 2005 have been made among the hazard factors, particularly those accounting for observed eruptive activity or unrest. The very low threat category underwent the greatest amount of change, dropping from 32 to 21 volcanoes, owing to better knowledge of the eruptive histories of those volcanoes. The list of 18 very high threat volcanoes determined by Ewert and others (2005) remains the same; 11 of the 18 volcanoes are located in Washington, Oregon, or California, where explosive and often snow- and ice-covered edifices can project hazards long distances to densely populated and highly developed areas. Five of the 18 very high threat volcanoes are in Alaska near important population centers, economic infrastructure, or below busy air traffic corridors. The remaining two very high threat volcanoes are on the Island of Hawaiʻi, where densely populated and highly developed areas now exist on the flanks of highly active volcanoes. The high- and moderate-threat categories are dominated by Alaskan volcanoes. In these categories the generally more active and more explosive volcanoes in Alaska can have a substantial effect on national and international aviation, and large eruptions from any of the moderate- to very-high-threat volcanoes could cause regional or national-scale disasters. This revised threat assessment includes 18 very high threat, 39 high threat, 49 moderate threat, 34 low threat, and 21 very low threat volcanoes. The total of 161 volcanoes is a decrease of 8 from the total reported by Ewert and others (2005).