In Fontana we often encounter a distinct velocity contrast at relatively shallow depths — alluvial fan deposits from the San Gabriel Mountains overlying older Tertiary sediments, with the Sierra Madre Fault Zone just to the north. This geological setting means that a generic VS30 value from a regional map won't capture the real seismic response of your site. We deploy active-source MASW with 24-channel seismographs and 4.5 Hz geophones, processed through dispersion curve inversion, to deliver a measured shear wave velocity profile tied directly to ASCE 7-22 Site Class. For sites with deep bedrock, we supplement the surface wave data with a targeted SPT drilling campaign to correlate N-values with velocity at depth, ensuring the profile is defensible for the reviewing structural engineer.
A measured VS30 of 360 m/s versus a default 260 m/s can reduce base shear demand by 20 percent — that's the difference between a mat foundation and a deep pile system.
