Santa Ana's growth from a small agricultural settlement in 1869 to Orange County's second-largest city means we now build on a complex patchwork of older alluvium and younger floodplain deposits. The Santa Ana River has shaped our subsurface over millennia, and with the Newport-Inglewood Fault just 12 miles to the southwest, seismic hazard is a daily design constraint. A generic code-based spectrum often misses what a seismic microzonation reveals: site-specific amplification, basin edge effects, and zones where the groundwater table fluctuates seasonally. We run the field campaigns and lab testing that feed directly into these maps, integrating shear wave velocity profiles with our MASW surveys to capture the stiffness contrast that drives site response in neighborhoods like Floral Park versus the Civic Center.
A site class D from a proxy map gets you in the ballpark. A microzonation gives you the actual ground motion at your foundation elevation, and in Santa Ana that can shave 15-20% off your seismic base shear.
