
Cascadia Subduction Zone Begins to Tear Itself Apart, Scientists Say
Scientists using the CASIE21 seismic program off Vancouver Island captured the Juan de Fuca plate tearing into fragments as it sinks beneath North America—a gradual, piecewise breakup with major tears (including a ~5 km drop and a ~75 km fault) that helps explain ancient plate remnants and will refine Cascadia earthquake hazard models. Despite these changes, the region remains capable of large earthquakes and tsunamis, though models will improve by incorporating the new details.



