The 18 March 2020 M w 5.7 Magna earthquake near Salt Lake City, Utah, offers a rare glimpse into the subsurface geometry of the Wasatch fault system-one of the world's longest active normal faults and a major source of seismic hazard in northern Utah. We analyze the Magna earthquake sequence and resolve oblique-normal slip on a shallow (30-35°) west-dipping fault at~9-to 12-km depth. Combined with near-surface geological observations of steep dip (~70°), our results support a curved, or listric, fault shape. High-precision aftershock locations show the activation of multiple, low-angle (<30-35°) structures, indicating the existence of a complicated fault system. Our observations constrain the deep structure of the Wasatch fault system and suggest that ground shaking in the Salt Lake City region in future Wasatch fault earthquakes may be higher than previously estimated. Plain Language Summary On 18 March 2020, a moment magnitude (M w) 5.7 earthquake occurred beneath Magna, Utah, a suburb of Salt Lake City. It was the largest earthquake in the Wasatch fault system in historical times, and shaking was felt throughout northern Utah. The mainshock and its aftershocks were located in the middle of a dense seismic network, generating a rare and valuable data set of strong ground accelerations from normal-faulting earthquakes. We analyzed the first~6 weeks of seismic data following the mainshock and found that the aftershocks formed a shallow-dipping planar structure at depths of 9-12 km, implying that this segment of the Wasatch fault zone has a curved shape. At the surface, it dips steeply to the west at~70°, but as the depth increases, the dip becomes progressively more shallow. Simulations of ground shaking from large earthquakes previously assumed that this fault segment was planar and steeply dipping (~50°) throughout the upper crust. Our observations suggest that the rupture area of future large earthquakes will be closer to the surface than previously thought, which would cause increased ground shaking in the Salt Lake City metropolitan area with its~1.2 million residents. Geological mapping and modeling of the WFZ finds near-surface dips of 45-90°on the SLCS (Bruhn et al., 1992); however, there are competing models for its subsurface structure under the Salt Lake ©2020. American Geophysical Union. All Rights Reserved.