MessageToEagle.com - A University of Utah seismologist analyzed seismic waves that bombarded Earth’s
core, and believes he got a look at the earliest roots of Earth’s most cataclysmic kind of volcanic eruption.
But don’t worry. He says it won’t happen for perhaps 200 million years.
“What we may be detecting is the start of one of these large eruptive events that – if it ever happens – could
cause very massive destruction on Earth,” says seismologist Michael Thorne, the study’s principal author and an
assistant professor of geology and geophysics at the University of Utah.
But disaster is “not imminent,” he adds, “This is the type of mechanism that may generate massive plume eruptions,
but on the timescale of 100 million to 200 million years from now. So don’t cancel your cruises.”
The new study shows that two or more continent-sized “piles” of rock are colliding as they move at the bottom of Earth’s thick mantle and
atop the thicker core some 1,800 miles beneath the Pacific. That is creating a Florida-sized zone of partly molten
rock that may be the root of either of two kinds of massive eruptions far in the future.
– Hotspot plume supervolcano eruptions like those during the past 2 million years at Wyoming’s Yellowstone caldera,
which covered North America with volcanic ash.
– Gargantuan flood basalt eruptions that created “large igneous provinces” like the Pacific Northwest’s Columbia
River basalts 17 million to 15 million years ago, India’s Deccan Traps some 65 million years ago and the Pacific’s
huge Ontong Java Plateau basalts, which buried an Alaska-sized area 125 million to 199 million years ago.
“These very large, massive eruptions may be tied to some extinction events,” Thorne says. The Ontong eruptions
have been blamed for oxygen loss in the oceans and a mass die-off of sea life.
Since the early 1990s, scientists have known of the existence of two continent-sized “thermochemical piles”
sitting atop Earth’s core and beneath most of Earth’s volcanic hotspots – one under much of the South Pacific
and extending up to 20 degrees north latitude, and the other under volcanically active Africa.
Using the highest-resolution method yet to make seismic images of the core-mantle boundary, Thorne and colleagues
found evidence the pile under the Pacific actually is the result of an ongoing collision between two or more piles.
Where they are merging is a spongy blob of partly molten rock the size of Florida, Wisconsin or Missouri beneath
the volcanically active Samoan hotspot.
The study’s computer simulations “show that when these piles merge together, they may trigger the earliest stages
of a massive plume eruption,” Thorne says.
Seismic imaging uses earthquake waves to make images of Earth’s interior somewhat like X-rays make CT scan
pictures of the inside of the human body.
The new study assembled the largest set of data ever used to map the lower mantle in the Pacific region by using
4,221seismograms from hundreds of seismometers around the world that detected 51 deep earthquakes originating more
than 60 miles under the surface.
Click on image to enlarge
This map shows Earth’s surface superimposed on a depiction of what a new University of Utah study indicates is happening 1,800 miles deep at
the boundary between Earth’s warm, rocky mantle and its liquid outer core. Using seismic waves the probe Earth’s deep interior, seismologist Michael
Thorne found evidence that two continent-sized piles of rock are colliding as they move atop the core. The merger process isn’t yet complete, so
there is a depression or hole between the merging piles. But in that hole, a Florida-sized blob of partly molten rock -- called a “mega ultra
low velocity zone” -- is forming from the collision of smaller blobs on the edges of the continent-sized piles. Thorne believe this process is the
beginning stage of massive volcanic eruptions that won’t occur for another 100 million to 2100 million years. Credit: Michael S. Thorne, University
Thorne and colleagues looked for secondary earthquake shear waves known as S-waves that travel through much of the Earth,
hitting the core, and then convert to primary compressional waves or P-waves as they travel across the top of the core.
Then they convert back to S-waves as they re-enter the mantle and then reach seismometers. Thorne says the short bursts
of P-wave energy are very sensitive to detecting variations in the rock at the core-mantle boundary.
Thorne performed 200 days of supercomputer simulations at the University of Utah’s Center for High Performance
Computing and found the shapes that could best explain the seismic wave patterns that were observed.
The new study provided an unusual look at one of the most remote parts of the Earth, located about 1,800 miles
beneath the surface: the boundary between the planet’s molten outer core and its warm mantle rock, which has
convection movement that has been compared with a conveyor belt or slowly boiling tomato soup.
“We did hundreds of simulations for lots of different variations of what the Earth might look like at the core-mantle
boundary – the most simulations anybody has ever done to look at the core-mantle boundary structure,” Thorne says
At some places where oceanic and continental tectonic plates collide – such as offshore from the Pacific Northwest
to Alaska – the seafloor plate dives or “subducts” beneath the continent and plunges slowly into the mantle.
Thorne suspects subducting plates ultimately fall deep enough to help push the piles around on Earth’s core.
Previous studies have observed smaller blobs of rock, measuring perhaps 60-by-60 miles on the edges of the
continent-sized masses. Seismic shear waves move as much as 45 percent slower through these blobs – known
technically as ULVZs or “ultra low velocity zones” – indicating they may be spongy and partly molten.
Analysis of seismic waves passing through the core-mantle boundary reveals the Pacific pile really
represents two or more continent-sized piles slowly sliding atop the core and colliding so that partly molten blobs
on their edges are merging into the largest such blob or ULVZ ever observed – roughly the size of Florida, according to Thorne.
“My study might be the first to show actual seismic evidence that the piles are moving,” he says. “People who have
done previous simulations have suggested this. They are sitting atop the core and getting pushed around by overlying
mantle forces like subduction. They move around on the core somewhat like continental plates drift at Earth’s surface.”
“We are actually seeing that these piles are being shoved around,” Thorne says. “If hotspots actually are
generated near the core-mantle boundary, where they are being generated seems related to where these piles
and ULVZs are. So if we are pushing these piles around, we also are pushing around where hotspot volcanism
The research is published in in the journal Earth and Planetary Science Letters.
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