Tomographic inversion is applied to delay times from aftershocks of the 1986 ML5.9 North Palm Springs (NPS) earthquake to image 3‐D velocity variations within the northern Coachella Valley. P‐wave arrival times from 1074 earthquakes, with depths ranging from 3 to 20 km, were used as sources recorded by 12 portable and 4 permanent stations. Preliminary results show well‐defined high‐ and low‐velocity anomalies (2–7%) that correlate with the rupture distribution of the 1986 mainshock. At depths less than 8 km, a low‐velocity anomaly predominates between the two NE‐dipping Banning and Mission Creek faults. From 8 to 12 km in depth, where the NPS mainshock and most of the aftershocks occur, a high‐velocity anomaly is observed. This high‐velocity feature is interpreted as imaging the asperity responsible for the 1986 rupture; and suggests that velocity information may help to define important elements, such as asperities, that control fault rupture, and thus, may help to predict the location and si