Pomona sits at the eastern edge of the Los Angeles Basin, where the San Jose Fault runs through the city and the alluvial sediments of the Pomona Valley can mask dramatic lateral velocity changes within just a few hundred feet. ASCE 7 requires site class determination, and the IBC mandates that soft soil profiles be identified before structural design begins. Seismic tomography (refraction/reflection) gives us a continuous 2D or 3D image of compressional and shear wave velocities, so you can see exactly where the bedrock drops, where a paleochannel cuts through the site, or whether that high-velocity spike at 40 feet is a boulder or the top of the San Antonio formation. Our field crew runs 24- to 48-channel spreads with a weight-drop or accelerated impact source, and we process the data with iterative ray-tracing algorithms that honor the actual curved ray paths through the soil column.
For deeper targets, we combine refraction with a MASW survey to get a Vs30 profile that feeds directly into the site classification, or we integrate the velocity model with liquefaction assessments when the groundwater table is shallow in the western part of the city near the 71 freeway corridor.
A dipping refractor missed by a standard 115-foot spread can shift your foundation design from spread footings to deep piles—and nobody wants to discover that during excavation.



