Much of Santa Ana sits atop the Santa Ana River floodplain, where Holocene alluvium creates layers of silts and sands with occasional clay lenses that challenge shallow foundation design. Groundwater can appear as shallow as 25 to 30 feet in central parts of the city, directly impacting liquefaction susceptibility under the seismic demands of the Newport-Inglewood Fault. A Cone Penetration Test delivers a continuous, high-resolution log of tip resistance, sleeve friction, and pore pressure — exactly the data required to model these stratified deposits without the sample disturbance inherent in traditional drilling. We combine this real-time stratigraphy with shear wave velocity profiling to refine site class per ASCE 7, and then integrate the results into liquefaction trigger analyses that satisfy both IBC Chapter 18 and the local building official’s review requirements.
Continuous cone data cuts through Santa Ana's alluvial variability: three parameters per inch, zero sample disturbance, one decisive borehole.
