New way to estimate magma beneath Yellowstone supervolcano

"It is the coal in the furnace that's heating things up," said Peter Larson, a professor in the Washington State University School of the Environment. "It's heating up the boiler. The boiler is what explodes. This tells us what is heating the boiler."

Some 640,000 years have passed since the volcano's last major eruption. But it can be "super," having produced one of the largest known blasts on Earth and spewing more than 2,000 times as much ash as Mount St. Helens did in 1980.

A major element in the volcano's power is the explosive, silica-rich rhyolite that break's through the Earth's crust during an eruption. Larson and his colleagues focused on the plume of basalt magma heating the rhyolite from below.

"This gives us an idea of how much magma is recharging the volcano every year," said Larson, whose findings appear in the latest issue of the journal Geosphere.

With funding from the National Science Foundation, the researchers "spiked" several hot springs in Yellowstone National Park with deuterium, a stable hydrogen isotope. The researchers used the length of time needed for deuterium concentrations to return to background levels and the temperature of the hot springs to calculate the amount of water and heat flowing out of the springs. Using deuterium for estimating heat flow is safe for the environment and has no visual impact to distract from the park visitors' experience.

The team found that previous studies underestimated the amount of water coursing through the springs and the amount of heat leaving the springs. The data also allowed the team to estimate the amount of magma entering the supervolcano from the mantle.

The study also has implications for geothermal energy, helping inform how heat is transported to the earth's surface from molten rock.