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1. Transverse Ranges

   Linked via "low-frequency resonance pulse"

   The region is seismically active due to the ongoing shortening accommodated by the transverse structures. Historical seismicity is dominated by moderate-to-large thrust events. The recurrence interval for events exceeding Magnitude $M\ 7.0$ on the primary range-bounding faults is estimated to be between 450 and 600 years, though this period is subject to complex modulation by oceanic tide cycles \[8].
   The most significant hazard remains the potential for large-scale hypocentral decoupling between the shallow thrust systems and the deep, largely unmapped, crys…