Lukewarm Supervolcano

Categories: Geology

Molten plume of material beneath Yellowstone cooler than expected

The Yellowstone volcano’s caldera, or sunken floor, covers an immense area.
Credit: U.S. Geological Survey

The geysers of Yellowstone National Park owe their existence to the "Yellowstone hotspot"–a region of molten rock buried deep beneath Yellowstone, geologists have found. But how hot is this "hotspot," and what’s causing it?

In an effort to find out, Derek Schutt of Colorado State University and Ken Dueker of the University of Wyoming took the hotspot’s temperature. The scientists published results of their research, funded by the National Science Foundation (NSF)’s division of earth sciences, in the August, 2008, issue of the journal Geology.

"Yellowstone is located atop of one of the few large volcanic hotspots on Earth," said Schutt. "But though the hot material is a volcanic plume, it’s cooler than others of its kind, such as one in Hawaii."

The ‘supervolcano’ of Yellowstone provides thermal heat for numerous hot springs. This hot spring vent in Yellowstone National Park is an example of an environment in which thermophilic archaea can thrive. Maximum vent temperature is approximately 74 degrees.
Credit: Jack Farmer

When a supervolcano last erupted at this spot more than 600,000 years ago, its plume covered half of today’s United States with volcanic ash. Details of the cause of the Yellowstone supervolcano’s periodic eruptions through history are still unknown. Thanks to new seismometers in the Yellowstone area, however, scientists are obtaining new data on the hotspot. Past research found that in rocks far beneath southern Idaho and northwestern Wyoming, seismic energy from distant earthquakes slows down considerably.

Using the recently deployed seismometers, Schutt and Dueker modeled the effects of temperature and other processes that affect the speed at which seismic energy travels. They then used these models to make an estimate of the Yellowstone hotspot’s temperature. They found that the hotspot is "only" 50 to 200 degrees Celsius hotter than its surroundings.

"Although Yellowstone sits above a plume of hot material coming up from deep with the Earth, it’s a remarkably ‘lukewarm’ plume," said Schutt, comparing Yellowstone to other plumes.

Although the Yellowstone volcano’s continued existence is likely due to the upwelling of this hot plume, the plume may have become disconnected from its heat source in Earth’s core.

"Disconnected, however, does not mean extinct," said Schutt. "It would be a mistake to write off Yellowstone as a ‘dead’ volcano. A hot plume, even a slightly cooler one, is still hot."

The reddish color of this geyser pool near Yellowstone’s Norris Geyser Basin may be due, in part, to iron-oxidizing bacteria living in its heated waters.
Credit: Idaho National Laboratory

In the past, supervolcanos on Earth may have been responsible for large-scale changes in climate and mass extinctions at the Earth’s surface. Some scientists even believe that a large volcanic eruption may have played a role in the extinction of the dinosaurs. Research on supervolcanos will help us understand how giant eruptions may have affected the evolution of life in our planet’s past – and what a future eruption could mean for life now.

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