“…However, ruptures may span multiple nearby fault segments (e.g., Landers earthquake, Li et al., 1994; and Hector Mine earthquake, Treiman et al., 2002) such that the maximum fault length is not a reliable predictor of the maximum earthquake magnitude. Such co‐slipping of en‐echelon fault systems has been observed for induced seismicity in Alberta, Canada (M W 4.1, Wang et al., 2018) and east Texas (M 4.8, Wang, Ellsworth et al., 2020). Within the Raton Basin, the largest earthquake since the beginning of injection was the M W 5.3 Trinidad event with a geodetically estimated rupture length of ∼8–10 km (Barnhart et al., 2014), which is shorter than the ∼14 km total length of the Trinidad zone of seismicity (Meremonte et al., 2002; Rubinstein et al., 2014).…”