“…Numerous studies assessing offshore Quaternary fault slip rates, offset, geometry, and seismic activity have been conducted over the past several decades. Detailed studies exist along the Newport‐Inglewood‐Rose Canyon fault (e.g., Sahakian et al., 2017; Singleton et al., 2021), the Carlsbad/San Onofre/San Mateo fault zone (Conrad et al., 2019; Holmes et al., 2021; Wei et al., 2020), the Palos Verdes fault (e.g., Alongi et al., 2022; Brothers et al., 2015) the San Diego Trough fault (e.g., H. F. Ryan et al., 2012), and the San Clemente fault (e.g., Walton, Brothers, et al., 2020), amongst others (e.g., Astiz & Shearer, 2000; Chaytor et al., 2008; Fisher et al., 2004; Lee et al., 2009; Legg et al., 2007, 2015; Lindvall and Rockwell, 1995; Pinter & Sorlien, 1991; H. F. Ryan et al., 2009; Seeber & Sorlien, 2000; Shaw & Suppe, 1996). Most of the documented Quaternary faults are considered to be seismically active today (e.g., Walton, Papesh, et al., 2020 data compilation).…”