Researchers from the University of Utah and the University of New Mexico used artificial “earthquakes” to investigate the magma beneath Yellowstone, a closely monitored hypervolcano. The team deployed truck-mounted bibroseis, large mechanical vibrators, to generate seismic waves throughout the national park. By recording these waves with 650 ground sensors, scientists were able to examine the underground volcanic structures.

Dr. Jamie Farrell, a geologist at the University of Utah and study co-author, explained, “In a way, we’re causing our own earthquakes and recording all that data on seismometers. With so many sensors, we can obtain a clear image of what’s happening below the surface.” This investigation revealed that the top of the magma chamber is approximately 3.8 km below the surface, with 86% consisting of solid rock and 14% containing molten rock, gas, and liquid pockets.

Professor Bill McGuire, an expert in Geophysical and Climate Hazards, noted that using artificial seismic waves to study underground geology is not new but has not been applied in Yellowstone for determining magma depth before. Despite the proximity of the magma to the surface, the study confirmed that an eruption is not imminent.

Mike Poland, the chief scientist at the US Geological Survey and Yellowstone Volcano Observatory, remarked, “Yellowstone provides valuable insights into volcano behavior worldwide. While another super eruption is possible elsewhere, Yellowstone is not currently at risk.”

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About our experts:

Professor Bill McGuire: Professor Emeritus of Geophysics and Climate Hazards at University College, London. McGuire is a science writer and broadcaster with a forthcoming book on how past events shape our future.