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The discovery and imaging of a mammoth magma reservoir beneath the Yellowstone supervolcano is a capstone to decades of research. Scientists have long known of a smaller magma chamber, but the new chamber – 4.4 times larger – helps answer the questions about the volcanic system.

Recent geophysical results suggest that two distinct magma chambers exist: a shallow, presumably felsic chamber and a deeper and much larger partially molten chamber above the Moho. To which extend the material parameters influence the rise of magma, the formation of shear zones in such systems and the magnitude of uplift remains puzzling.

Aug 17, 2023 · Researchers at the University of Utah and the University of New Mexico chose over 600 locations in Yellowstone National Park to get a better understanding of the magma chamber.

Apr 23, 2015 · To create an "image" of the magma storage region (reservoir) beneath Yellowstone, the research teams reviewed data from thousands of earthquakes. Seismic waves travel slower through hot, partially molten rock and faster in cold, solid rock.

Apr 17, 2013 · Scientists have updated this image of Yellowstone volcano's underground magma chamber. Instead of two big yellow blobs, they have a clearer picture that looks like a knobby banana.

Jan 14, 2025 · Seismic imaging of the Yellowstone system has also identified a deeper magma body, likely composed of basalt—Earth’s most primitive magma type and the heat engine that helps to generate and sustain the shallower rhyolite magma chamber.

University of Utah seismologists discovered and made images of a reservoir of hot, partly molten rock 12 to 28 miles beneath the Yellowstone supervolcano, and it is 4.4 times larger than the...

4 days ago · The volcano has had no lava eruption for 70,000 years and no major eruption for 631,000 years, however.The volcano's magma chamber between 5 and 10 miles under the surface heats the underground ...

4 days ago · Yellowstone National Park has a new thermal vent spewing steam in the air that could be visible to tourists once visitors flock back into the park ... The volcano's magma chamber between 5 and 10 ...

The Yellowstone magmatic system is one of the largest magmatic systems on Earth. Recent seismic tomography suggest that two distinct magma chambers exist: a shallow, presumably felsic chamber and a deeper much larger, partially molten, chamber above the Moho.

Jul 31, 2023 · Data from a major deployment of seismometers in 2020 is revealing new insights into the characteristics of the magma chamber beneath Yellowstone caldera, including how melt is distributed in the reservoir.

4 days ago · The volcano's magma chamber between 5 and 10 miles (8 and 16 kilometers) under the surface heats the underground water that bubbles up as the park's famous hydrothermal features. ... Only between ...

April 23, 2015 – University of Utah seismologists discovered and made images of a reservoir of hot, partly molten rock 12 to 28 miles beneath the Yellowstone supervolcano, and it is 4.4 times larger than the shallower, long-known magma chamber.

Apr 23, 2015 · Geoscientists have now completely imaged the subterranean plumbing system and have found not just one, but two magma chambers underneath the giant volcano. "The main new thing is we unveil a deeper and bigger magma reservoir in the lower crust," says study author Hsin-Hua Huang, a seismologist at the University of Utah in Salt Lake City.

4 days ago · Yellowstone National Park has a new thermal vent spewing steam in the air that could be visible to tourists once visitors flock back into the park. ... The volcano’s magma chamber between 5 and 10 miles (8 and 16 kilometers) under the surface heats the underground water that bubbles up as the park’s famous hydrothermal features. ...

1 day ago · Yellowstone’s thermal features come and go, but Old Faithful Geyser is still going strong. ... The volcano's magma chamber between 5 and 10 miles (8 and 16 kilometers) under the surface heats ...

How big is the magma chamber under Yellowstone? Yellowstone is underlain by two magma bodies. The shallower one is composed of rhyolite (a high-silica rock type) and stretches from 5 km to about 17 km (3 to 10 mi) beneath the surface and is about 90 km (55 mi) long and about 40 km (25 mi) wide.