Mount St. Helens Is Recharging: What Rising Magma Means

Mount St. Helens, as viewed from Elk Rock, in Washington state.
Mount St. Helens, as viewed from Elk Rock, in Washington state.
(Image credit: Liz Westby)

ANCHORAGE, Alaska — Mount St. Helens is nowhere near another eruption, but new magma is rising underground, heaving the volcano upward and outward by the length of a fingertip, researchers said here today (May 2) at the annual meeting of the Seismological Society of America.

A small amount of magma started pooling 2.5 to 3 miles (4 to 5 kilometers) beneath the volcano in 2008, said lead study author Seth Moran, a seismologist with the Cascades Volcano Observatory in Washington state. The depth comes from the pattern of surface swelling, measured with GPS, and from earthquakes triggered by the molten rock pushing upward. GPS units moved away from the center of the volcano by up to 0.5 inches (12 millimeters) between 2008 and 2013. (Imagine that Mount St. Helens' magma chamber is like a balloon inflating deep beneath the volcano, pushing everything above it out of the way as it fills with a fresh batch of molten rock.) [Gallery: The Incredible Eruption of Mount St. Helens]

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Becky Oskin
Contributing Writer
Becky Oskin covers Earth science, climate change and space, as well as general science topics. Becky was a science reporter at Live Science and The Pasadena Star-News; she has freelanced for New Scientist and the American Institute of Physics. She earned a master's degree in geology from Caltech, a bachelor's degree from Washington State University, and a graduate certificate in science writing from the University of California, Santa Cruz.