Documented: the Juan de Fuca plate, with its Explorer and Gorda microplates, subducts beneath North America at a few centimeters per year and generates the CSZ's lock. Recent seismic imaging studies (2024-2026 coverage) report tears and fragmentation in the descending slab, holes and breaks where pieces peel away, which alters stress transfer and may explain the zone's anomalous quiet and segment boundaries.
The folk delight: Juan de Fuca, born Apostolos Valerianos, claimed a strait in 1592 that later mapmakers chased for two centuries, and the plate bears the name of a man whose discovery is documented mostly as a story told to a stranger in Venice. The coast's geology is thus named after its mythology.
The claim, from the fringe seismic channels: the tearing slab is the setup for a cascading rupture, plate fragmentation as the mechanism behind the double whammy scenario and worse. The measured version: fragmentation may bound ruptures as easily as chain them.
If the plate is tearing as it sinks, does the next big one arrive as one blow or a burst?