Yellowstone magma discovery
A team of University of Utah seismologists has discovered a reservoir of hot, partly molten rock hidden 12 to 28 miles beneath Yellowstone National Park's supervolcano--enough to fill the 1000 cubic-mile Grand Canyon more than 11 times. The pool is over four times larger than a shallower, long-known magma chamber. The National Science Foundation (NSF)-funded team developed a new technique that uses both local and distant earthquake data from the university's seismograph stations and the NSF-funded EarthScope array of seismometers. The combined data resulted in a better, deeper and more complete image of the system. The newly discovered reservoir carries hot and partly molten rock upward from the top of Yellowstone's hotspot plume--about 40 miles below the surface. Yellowstone's plumbing system is no larger or closer to erupting than before the discovery. It's just that scientists are now seeing more of the plumbing system than ever before. The team believes these new models help us gain a better understanding of Yellowstone's plumbing system, and may lead to improved estimates of the potential future seismic and volcanic hazards.
Provided by the National Science Foundation