Mount St. Helens, in southwestern Washington, is one of the many steep-sided and often snow-covered stratovolcanoes, otherwise known as composite volcanos, that line the Cascade Range. “It actually looked really similar to a lot of the other stratovolcanoes,” says Jessica L. Ball, volcano hazards and communication specialist at the USGS California Volcano Observatory. “It was considered one of the most beautiful and symmetrical.”
That all changed, of course, on May 18, 1980, when, after two months of earthquakes and steam explosions, Mount St. Helens violently erupted, blowing its own top off and spewing massive quantities of debris across a 230 square mile blast zone. As an ash cloud from the eruption began circling the globe, mudflows choked the Toutle River and other waterbodies, bulldozing everything in their path and behaving “like a flood of wet concrete,” Ball explains.
In the end, 57 people died in the eruption, including scientists, loggers, campers and journalists, most from thermal burns or inhaling hot ash. Hundreds of buildings were destroyed, along with bridges, and vast tracts of forest were wiped out.
Scientists learned a lot from the eruption, Ball says, noting “they weren’t expecting the sideways blasts to happen.”
Today, the landscape around Mount St. Helens is gradually recovering. “It’s a lot greener, there’s a lot more larger plants establishing themselves, there’s probably a lot more wildlife in those places,” Ball says. “It’s definitely happening on a human timescale.”
Even so, another eruption is expected at some point. In a 2018 report, the USGS ranked Mount St. Helens as posing a greater threat than all but one other U.S. volcano. Additional high-threat volcanoes in Washington include Mount Rainier, Mount Baker and Glacier Peak.