Scientists have mapped one of the most hazardous spots on the globe in unprecedented detail: a 600-mile geologic boundary just off the Pacific Northwest coast.

Brian Agee deploys the streamer, a 9-mile-long cable embedded with specialized microphones, from the research vessel Marcus G. Langseth in summer of 2021. The craft is trying to map the Cascadia subduction zone off the coast of the Pacific Northwest. (Madeleine Lucas/University of Washington )

By Carolyn Y. Johnson, The Washington Post

Scientists have mapped one of the most hazardous spots on the globe in unprecedented detail: a 600-mile geologic boundary just off the Pacific Northwest coast.

Along this fraught stretch, called the Cascadia subduction zone, two pieces of the Earth’s crust slide against each other, building up stresses capable of unleashing a catastrophic 9.0-magnitude earthquake and generating a tsunami, with waves as high as 40 feet.

Because scientists don’t know when that day will arrive, they prepare by trying to better understand the geological state of play.

The Marcus G. Langseth, a 235-foot research vessel equipped to conduct seismic research. (Harold Tobin/University of Washington )

To do that, a 235-foot ship cruised for 41 days along the coast of Oregon, Washington and British Columbia in summer of 2021, sending sound waves deep into the ocean and recording the echoes with a “streamer” — a 9-mile-long waterproof cable containing 1,200 specialized microphones. Similar to how doctors use ultrasound to see inside the body, they used the data to construct a comprehensive map of the underwater geology in a study published Friday in the journal Science Advances. The new resource will help scientists understand the range of earthquake and tsunami scenarios — and help policymakers devise building codes that protect people.

Because scientists don’t know when that day will arrive, they prepare by trying to better understand the geological state of play.

The entire area, which stretches from Northern California to Vancouver Island, is at risk. But the scientists found that the geometry of the fault

off the coast of Washington, where the fault is flat and smooth, closer to the surface and extends farther onshore, may be particularly at risk.

“I’m excited to use these results to make sure the shaking estimates I’m producing are as accurate as they can be,” said Erin Wirth, a seismologist with the United States Geological Survey who was not involved in the study. “I’ll be busy now.”

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