It looks like you're using an Ad Blocker.
Please white-list or disable AboveTopSecret.com in your ad-blocking tool.
Thank you.
Some features of ATS will be disabled while you continue to use an ad-blocker.
The explosives are just part of researchers at iMUSH‘s (or Imaging Magma Under St. Helens) plan to map out something that has never been seen: the magma chambers that feed Mount St. Helens
• iMUSH (“imaging Magma Under St. Helens”) is a project to improve volcano monitoring and aims to save lives by learning more about the underground feeder system that supplies magma to Mount St. Helens (MSH).
• The project will collect new data, via minimum-impact temporary instrument deployments, to produce high-resolution images of the Earth beneath Mount St. Helens. The scientists will integrate these images with existing geologic datasets to develop improved models of the Mount St. Helens magma systems.
• The deployments will collect magnetotelluric (MT), passive-source seismic and active-source seismic data, details below.
• Such a large-scale and multidisciplinary integrated approach has rarely been attempted at volcanoes due to expense and difficult logistics, but is critical for forming a high-resolution three-dimensional model of the Earth to the necessary depth of 60 miles.
• Our integrated approach will produce a state-of-the art high-resolution image that will allow unambiguous interpretations and improved understanding of the volcano’s inner workings, which will help us do more effective above-ground monitoring of Mount St. Helens.
Some people may wonder if explosive sources might "wake up" the volcano or do other damage to the area. Actually, such events are not at all unusual and of course none of these have any chance what so ever of effecting volcanic activity of any type. The amount of explosives used in our case is small, smaller than typical explosions in the region for other purposes that take place many days of the year.
originally posted by: MOMof3
a reply to: Observationalist
I applaud their cause, since that is my neighborhood. Still, the thought keeps going through my mind, "what could go wrong?".
originally posted by: MOMof3
a reply to: Observationalist
I applaud their cause, since that is my neighborhood. Still, the thought keeps going through my mind, "what could go wrong?".
• Such a large-scale and multidisciplinary integrated approach has rarely been attempted at volcanoes due to expense and difficult logistics, but is critical for forming a high-resolution three-dimensional model of the Earth to the necessary depth of 60 miles.
Of course we can't dig down deep in the earth to see what is actually there (drilling can only reach depths of 5+ km and at those depths is incredibly expensive and only samples that one place). But, we can let the rocks come to us. They do so in eruptions and Mount St. Helens has brought up all sorts of rocks during the eruptions that have taken place during the past 32 years
(9) there are long-standing working relations between the academic community, government agencies and land managers that will facilitate permitting of instruments and leveraging of extensive existing resources.
“E2I sprang partly from a realization that Rice is already doing excellent energy-related research and education,” McLendon said. “We have significant federal support for research on topics as diverse as enhanced oil recovery, carbon sequestration and next-generation solar power. Rice’s research in energy economics and energy policy is globally recognized. Our top-ranked Jones Graduate School of Business serves the energy industry through its MBA concentration in energy and its executive education program. We have existing relationships with companies such as Shell, Chevron, ExxonMobil, BP, Total, Baker Hughes, Schlumberger and Apache. Finally, Rice partnered with the Mellon Foundation last year to pioneer the field of ‘energy humanities’ research.” - See more at: news.rice.edu...
The Mellon family is a wealthy and influential family originally of Pittsburgh, Pennsylvania, United States, and its vicinity. The center of the family fortune was Mellon Bank founded 1869 and growing into one of America's largest before its 2007 merger into the Bank of New York Mellon. From the family's base in banking and finance they became principal investors and majority owners of Gulf Oil (founded 1901 becoming Chevron-Texaco in 1985), Alcoa (since 1886),
That would be cool to see.
Results show that on one side the mantle is largely serpentinite, a rare, moisture-absorbing, dark-green mineral that can look like a snake’s skin.
But the mantle below the eastern half of the mountain is mostly olivine, a common mineral that allows water—thought to play a key role in volcanic eruptions—to percolate up and into the overlying crust.
Water is locked in various minerals inside the subducting oceanic plate. As the slab goes down, the temperature and pressure increase and the water is squeezed out of the crystals. The water then migrates up into the mantle of the overriding continental plate, where it reacts with olivine to become serpentinite to the west of Mount St. Helens, or olivine to the east. The temperature is key, Creager says, because that indicates where water in the descending ocean plate could be mixing with the rock to lower the melting temperature and form volcano-creating magma
“An important question is: where is the water, and where isn’t it?” Creager says
Wiki
The abundance of gases varies considerably from volcano to volcano. Water vapor is consistently the most common volcanic gas, normally comprising more than 60% of total emissions. Carbon dioxide typically accounts for 10 to 40% of emissions.
originally posted by: Observationalist
UPDATE:
Here is an article that posts the results of the IMUSH experiment.
That would be cool to see.
Results show that on one side the mantle is largely serpentinite, a rare, moisture-absorbing, dark-green mineral that can look like a snake’s skin.
Water?
But the mantle below the eastern half of the mountain is mostly olivine, a common mineral that allows water—thought to play a key role in volcanic eruptions—to percolate up and into the overlying crust.
Where did the water come from?
Water is locked in various minerals inside the subducting oceanic plate. As the slab goes down, the temperature and pressure increase and the water is squeezed out of the crystals. The water then migrates up into the mantle of the overriding continental plate, where it reacts with olivine to become serpentinite to the west of Mount St. Helens, or olivine to the east. The temperature is key, Creager says, because that indicates where water in the descending ocean plate could be mixing with the rock to lower the melting temperature and form volcano-creating magma
Now what?
“An important question is: where is the water, and where isn’t it?” Creager says
Why it's important
Wiki
The abundance of gases varies considerably from volcano to volcano. Water vapor is consistently the most common volcanic gas, normally comprising more than 60% of total emissions. Carbon dioxide typically accounts for 10 to 40% of emissions.
There you go and update if anyone cared.