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⚠️ PACIFIC NORTHWEST 9.0 MEGAQUAKE RISK The Cascadia Subduction Zone is a 1,000 km megathrust fault off the coasts of Vancouver Island, Washington, Oregon and northern California. Geological records from drowned forests, sand sheets and offshore cores show that Cascadia has produced many great earthquakes over the last 10,000 years, with full-margin ruptures repeating on the order of hundreds of years. A new line of research looks at the relationship between Cascadia and the San Andreas Fault. A
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Subduction zone earthquakes occur when tectonic plates converge, and one plate is forced beneath another, creating immense stress along the fault interface. Over decades or even centuries, strain accumulates until the rocks can no longer withstand the pressure, resulting in a sudden, violent slip that releases energy as a megathrust earthquake. These earthquakes are among the most powerful on Earth, with recurrence intervals ranging from hundreds to thousands of years, depending on the subductio
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