WA Ping It looks like we have two different threads going. I'm pinging the one with the most comments.
Posted on 07/18/2014 9:45:32 AM PDT by JimSEA
July 17, 2014 – By measuring how fast Earth conducts electricity and seismic waves, a University of Utah researcher and colleagues made a detailed picture of Mount Rainier’s deep volcanic plumbing and partly molten rock that will erupt again someday.
“This is the most direct image yet capturing the melting process that feeds magma into a crustal reservoir that eventually is tapped for eruptions,” says geophysicist Phil Wannamaker, of the university’s Energy & Geoscience Institute and Department of Civil and Environmental Engineering. “But it does not provide any information on the timing of future eruptions from Mount Rainier or other Cascade Range volcanoes.”
The study was published today in the journal Nature by Wannamaker and geophysicists from the Woods Hole Oceanographic Institution in Massachusetts, the College of New Jersey and the University of Bergen, Norway.
In an odd twist, the image appears to show that at least part of Mount Rainier’s partly molten magma reservoir is located about 6 to 10 miles northwest of the 14,410-foot volcano, which is 30 to 45 miles southeast of the Seattle-Tacoma area.
But that could be because the 80 electrical sensors used for the experiment were placed in a 190-mile-long, west-to-east line about 12 miles north of Rainier. So the main part of the magma chamber could be directly under the peak, but with a lobe extending northwest under the line of detectors, Wannamaker says.
The top of the magma reservoir in the image is 5 miles underground and “appears to be 5 to 10 miles thick, and 5 to 10 miles wide in east-west extent,” he says. “We can’t really describe the north-south extent because it’s a slice view.”
Wannamaker estimates the reservoir is roughly 30 percent molten. Magma chambers are like a sponge of hot, soft rock containing pockets of molten rock.
The new image doesn’t reveal the plumbing tying Mount Rainier to the magma chamber 5 miles below it. Instead, it shows water and partly molten and molten rock are generated 50 miles underground where one of Earth’s seafloor crustal plates or slabs is “subducting” or diving eastward and downward beneath the North America plate, and how and where those melts rise to Rainier’s magma chamber.
The study was funded largely by the National Science Foundation’s Earthscope program, which also has made underground images of the United States using seismic or sound-wave tomography, much like CT scans show the body’s interior using X-rays.
The new study used both seismic imaging and magnetotelluric measurements, which make images by showing how electrical and magnetic fields in the ground vary due to differences in how much underground rock and fluids conduct or resist electricity.
Wannamaker says it is the most detailed cross-section view yet under a Cascades volcanic system using electrical and seismic imaging. Earlier seismic images indicated water and partly molten rock atop the diving slab. The new image shows melting “from the surface of the slab to the upper crust, where partly molten magma accumulates before erupting,” he adds.
Wannamaker and Rob L. Evans, of the Woods Hole Oceanographic Institution, conceived the study. First author R Shane McGary – then at Woods Hole and now at the College of New Jersey – did the data analysis. Other co-authors were Jimmy Elsenbeck of Woods Hole and Stéphane Rondenay of the University of Bergen.
Mount Rainier: Hazardous Backdrop to Metropolitan Seattle-Tacoma
Mount Rainier, the tallest peak in the Cascades, “is an active volcano that will erupt again,” says the U.S. Geological Survey. Rainier sits atop volcanic flows up to 36 million years old. An ancestral Rainier existed 2 million to 1 million years ago. Frequent eruptions built the mountain’s modern edifice during the past 500,000 years. During the past 11,000 years, Rainier erupted explosively dozens of times, spewing ash and pumice.
Rainier once was taller until it collapsed during an eruption 5,600 years ago to form a large crater open to the northeast, much like the crater formed by Mount St. Helens’ 1980 eruption. The 5,600-year-old eruption sent a huge mudflow west to Puget Sound, covering parts or all of the present sites of the Port of Tacoma, Seattle suburbs Kent and Auburn, and the towns Puyallup, Orting, Buckley, Sumner and Enumclaw.
Rainier’s last lava flows were 2,200 years ago, the last flows of hot rock and ash were 1,100 years ago and the last big mudflow 500 years ago. There are disputed reports of steam eruptions in the 1800s.
The “ring of fire” is a zone of active volcanoes and frequent earthquake activity surrounding the Pacific Ocean. It exists where Earth’s tectonic plates collide – specifically, plates that make up the seafloor converge with plates that carry continents.
From Cape Mendocino in northern California and north past Oregon, Washington state and into British Columbia, an oceanic plate is being pushed eastward and downward – a process called subduction – beneath the North American plate. This relatively small Juan de Fuca plate is located between the huge Pacific plate and the Pacific Northwest.
New seafloor rock – rich with water in cracks and minerals – emerges from an undersea volcanic ridge some 250 miles off the coast, from northern California into British Columbia. That seafloor adds to the western edge of the Juan de Fuca plate and pushes it east-northeast under the Pacific Northwest, as far as Idaho.
The part of the plate diving eastward and downward is called the slab, which ranges from 30 to 60 miles thick as it is jammed under the North American plate. The part of the North American plate above the diving slab is shaped like a wedge.
When the leading, eastern edge of the diving slab descends deep enough, where pressures and temperatures are high, water-bearing minerals such as chlorite and amphibole release water from the slab, and the slab and surrounding mantle rock begin to melt. That is why the Cascade Range of active volcanoes extends north-to-south – above the slab and parallel but about 120 miles inland from the coast – from British Columbia south to Mount Shasta and Lassen Peak in northern California.
In the new image, yellow-orange-red areas correspond to higher electrical conductivity (or lower resistivity) in places where fluids and melts are located.
The underground image produced by the new study shows where water and molten rock accumulate atop the descending slab, and the route they take to the magma chamber that feeds eruptions of Mount Rainier:
– The rock begins to melt atop the slab about 50 miles beneath Mount Rainier. Wannamaker says it is best described as partly molten rock that contains about 2 percent water and “is a mush of crystals within an interlacing a network of molten rock.”
– Some water and partly molten rock actually gets dragged downward atop the descending slab, to depths of 70 miles or more.
– Other partly molten rock rises up through the upper mantle wedge, crosses into the crust at a depth of about 25 miles, and then rises into Rainier’s magma chamber – or at least the lobe of the chamber that crosses under the line of sensors used in the study. Evidence suggests the magma moves upward at least 0.4 inches per year.
The new magnetotelluric image also shows a shallower zone of fluid perhaps 60 miles west of Rainier and 25 miles deep at the crust-mantle boundary. Wannamaker says it is largely water released from minerals as the slab is squeezed and heated as it dives.
The seismic data were collected during 2008-2009 for other studies. The magnetotelluric data were gathered during 2009-2010 by authors of the new study.
Wannamaker and colleagues placed an east-west line of magnetotelluric sensors: 60 that made one-day measurements and looked as deep as 30 miles into the Earth, and 20 that made measurements for a month and looked at even greater depths.
The Energy & Geoscience Institute at the University of Utah employs more than 100 scientists and staff, and conducts the world’s largest, university-based, cost-shared research program focusing on oil, gas and geothermal exploration and production. The institute perhaps is known best for its international hydrocarbon research consortium sponsored by more than 70 global energy corporations. Wannamaker does research worldwide as a principal investigator in the institute’s geothermal group.
Interesting!
Good find.
Did you notice: 10 times it erupted in 10,000 years.
Last eruption was 1000 years ago.
It could go again at any time.
WA ping.
Just great— I’m flying at to Tacoma at the end of the month. Now I’ll have something else to worry about. :)
I see that sleeping giant big as life from my home only 35 miles away.
Are you east or west of it?
Indeed it could. In fact there are several Cascade / West Coast volcanos that could go anytime. This prediction method is a good thing.
I’ve always appreciated the beauty of Rainier. However, climbing on it and driving / hiking the adjacent area gives a person an appreciation of its potential.
I’m about 35 miles northwest of it in a town called Graham.
I hope you're joking. Unless you're engaged in a summit climb, or chained to the bottom of one of Rainier's lahar outflow channels, you have nothing much to worry about if you happen to be in the Puget Sound area during a typical once-in-a-thousand year Rainier eruption. Nothing like Mt. St. Helen's catastrophic 1980 eruption, which lead to a couple of weeks of work for me shoveling ash.
The government should try to do something about this situation.
But unless they can conjure up that it is manmade, and a way to tax it, it may not prove a fertile option to exploit.
What elevation did you reach? I can still hike a steep ascent ok but unfortunately my knees give out when starting down. Leads to some very awkward and potentially funny to watch descents.
It was quite a few years ago and I walked up to the glaciers, an easy walk, and lower down, into a very deep canyon eroded in the south side. Walking along one of the old lahars on the east side was a good way to appreciate their power. At this point some twenty five years later, I’d have to look at a map to get elevations and place names.
WA Ping It looks like we have two different threads going. I'm pinging the one with the most comments.
Washington Governor Jay Inslee would be perfectly happy to come up with a $10BILLION dollar fine for the ash and carbon discharge and then prorate it to every Washington resident. He's already proposing adding another $1.17 to our gas tax which is 2nd highest in the nation.
“Washington Governor Jay Inslee would be perfectly happy to come up with a $10BILLION dollar fine for the ash and carbon discharge and then prorate it to every Washington resident. He’s already proposing adding another $1.17 to our gas tax which is 2nd highest in the nation. “
George Harrison had it right in “Taxman.”
These clowns would tax breathing in and breathing out, if they could.
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