The Wasatch Fault Corridor in northern Utah (USA) faces increasing seismic risks due to rising population density. V_s30 is a vital parameter for understanding how a site will respond to earthquake shaking; however, obtaining V_s30 can be costly or impractical because of infrastructure or access challenges. The horizontal-to-vertical spectral ratio (HVSR) enables rapid assessment, provided a relationship between V_s30 and the resonant frequency (f₀) of the shallow subsurface can be established. Previously surveyed V_s30 sites in the Provo segment of the Wasatch Fault Zone were measured with a three-component seismometer to obtain f₀. These sites are located on the hanging wall of the fault zone, within alluvial and lacustrine Quaternary sediments. For each of the 20 sites, ambient noise was recorded for 30 minutes and amplitude-frequency spectra computed for each component. A rubric was applied to select site results most suitable for analysis and forward modelling, based on uncertainty of f₀, uncertainty of H/V response, and peak quality. The H/V response was then derived for 15 selected sites. The strongest low-frequency peak identified the f₀, which ranged from 0.28 to 1.38 Hz. Experimenting with linear regression helps guide understanding of the potential for estimating V_s30 from HVSR in this region.