The 2019 Ridgecrest earthquake sequence initiated on July 4th with a series of foreshocks that included an M w 6.4 event and culminated 34 h later with the M w 7.1 mainshock event. This sequence was also notable in that it resulted in rupture of a set of more than 20 cross-faults (Brandenberg et al., 2020; Ross et al., 2019; Xu et al., 2020). The earthquake sequence occurred within the northern region of the eastern California shear zone (ECSZ), a 150-km wide zone of NW-trending dextral shear that accommodates up to ∼20% of the North America-Pacific plate boundary motion (McClusky et al., 2001; Rockwell et al., 2000). Seismic and geodetic inversions show the M w 6.4 event likely ruptured multiple fault segments, where it initiated on a short NW-trending, dextral fault, and then propagated to the southwest along a series of parallel NE-trending sinistral faults for 16 km (