In October 2016, we acquired high-resolution P- and S-wave seismic data along a 120-m-long, SW-NE-trending profile in Napa, California.  Our seismic survey was designed to image a strand of the West Napa Fault Zone (WNFZ), which ruptured during the 24 August 2014 Mw 6.0 South Napa Earthquake.  We separately acquired P- and S-wave data at every station using multiple hammer hits, which were edited and stacked into individual shot gathers in the lab.  Each shot was co-located with and recorded by 118 P-wave (40-Hz) geophones, spaced at 1 m, and by 118 S-wave (4.5-Hz) geophones, spaced at 1 m.  We developed both P- and S-wave tomographic velocity models, as well as Poisson’s ratio and a Vp/Vs ratio models.   We observed a well-defined zone of elevated Vp/Vs ratios below about 10 m depth, centered beneath the observed surface rupture.   P-wave reflection images show that the fault forms a flower-structure in the upper few tens of meters.  This method has been shown to delineate fault structures even in areas of rough terrain.