The gorgeous colors of Yellowstone’s Grand Prismatic hot spring are among the national park’s myriad hydrothermal features created by the Yellowstone supervolcano. A new University of Utah study reports discovery of a huge magma reservoir beneath Yellowstone’s previously known magma chamber. (“Windows into the Earth,” Robert B. Smith and Lee J. Siegel)
On Thursday, a team from the University of Utah published a study, in the journal Science that for the first time offers a complete diagram of the plumbing of the Yellowstone volcanic system.
The new report fills in a missing link of the system. It describes a large reservoir of hot rock, mostly solid but with some melted rock in the mix, that lies beneath a shallow, already-documented magma chamber. The newly discovered reservoir is 4.5 times larger than the chamber above it. There's enough magma there to fill the Grand Canyon. The reservoir is on top of a long plume of magma that emerges from deep within the Earth's mantle.
[Geysers erupt because they’re all bendy inside]
This system has been in place for roughly 17 million years, with the main change being the movement of the North American tectonic plate, creeping at the rate of roughly an inch a year toward the southwest. A trail of remnant calderas can be detected across Idaho, Oregon and Nevada, looking like a string of beads, marking the migration of the tectonic plate. A similar phenomenon is seen in the Hawaiian islands as the Pacific plate moves over a hot spot, stringing out volcanoes, old to new, dormant to active.
University
of Utah seismologists funded by the National Science Foundation found a
pool of magma beneath Yellowstone's supervolcano that they say is big
enough to fill the Grand Canyon more than 11 times. (National Science
Foundation/University of Utah)
This new picture doesn't change, fundamentally, the risk assessment of Yellowstone, but it will help scientists understand the mechanics of the volcano.
“Really getting an idea of how it works and understanding how these large caldera-forming eruptions may occur, and how they might happen, would be a good thing to understand," said paper co-author Jamie Farrell, another geophysicist at the university. "No one's ever witnessed one of these really large volcanic eruptions. We kind of scale smaller eruptions up to this size and say, 'This is probably how it happens,' but we really don’t know that for sure.”
[What Yellowstone’s Thermal Springs looked like before humans contaminated them]
The next major, calderic eruption could be within the boundaries of the park, northeast of the old caldera.
“If you have this crustal magma system that is beneath the pre-Cambrian rocks, eventually if you get enough fluid in that system, enough magma, you can create another caldera, another set of giant explosions," Smith said. "There’s no reason to think it couldn’t continue that same process and repeat that process to the northeast.”
The report is based on the equivalent of an MRI of the crust beneath Yellowstone. Nature itself supplies the key diagnostic tool: Earthquakes. The Yellowstone region is seismically active, and in any given year there can be hundreds of small earthquakes. These tremors send seismic waves racing through the planet's crust. Seismographs stationed around Yellowstone and across the United States record the arrival of these waves and carefully measure how long it took for them to reach the instruments. The speed of the waves carries information: When the seismic waves hit hot rock, they go slower; when they pass through cold rock, they're faster. By combining the data from many sensors, scientists can get a picture of the hot and cold rock beneath Yellowstone. This is known as "seismic tomography."
This is a volcano that can erupt either in a big way or a truly colossal and catastrophic way. The big eruptions can send lava flowing over a big portion of the park; the really huge ones can form a giant crater, or caldera. The last time Yellowstone had a calderic eruption was 640,000 years ago, and the misshapen hole it created was about 25 miles by 37 miles across. This caldera has since been filled in by lava flows and natural erosion, and Yellowstone Lake covers a portion of the area. The main visual evidence of the old caldera is the striking absence of mountains at the heart of the park: They were literally blown away in the last eruption.
Risk assessment is tricky for low-probability, high-consequence events like volcanic eruptions. The big Yellowstone eruptions occur on time scales of many hundreds of thousands of years. Smith said the repeat time for a caldera explosion at Yellowstone is roughly 700,000 years. But the smaller eruptions, with lava flowing over the surface, are more frequent. There have been at least 50 such smaller eruptions since the caldera exploded 640,000 years ago. The most recent was about 70,000 years ago.
Geological processes don't follow clocks. These are chaotic systems, with strain building unpredictably as distant faults break and the geological stresses shift here and there.
Bottom line: Yellowstone is unpredictable. There's no sign at all that this old volcano is going to erupt anytime soon, either in a big way or a huge, show-stopper way. But neither is there any evidence that it's running out of steam.
A new study provides the first complete view of the plumbing system that supplies hot and partly molten rock from the Yellowstone hotspot to the Yellowstone supervolcano. The study revealed a gigantic magma reservoir beneath the previously known magma chamber. This cross-section illustration cutting southwest-northeast under Yellowstone depicts the view revealed by seismic imaging. Seismologists estimate the annual chance of a Yellowstone supervolcano eruption is 1 in 700,000. (Hsin-Hua Huang/University of Utah)
