Little Rock sits in a geologically layered transition zone where the Quaternary alluvium of the Arkansas River floodplain meets weathered Paleozoic shale and sandstone of the Ouachita foothills. The city’s ASCE 7 seismic design category demands more than just a generic site class assumption — it requires a measured VS30 value that captures how shear waves actually travel through the upper 30 meters. We run active-source MASW surveys with a 24-channel seismograph and 4.5 Hz geophones, extracting a dispersion curve that gets inverted into a 1D shear wave velocity profile. That profile feeds directly into the NEHRP site classification table, giving engineers a defensible Site Class between A and E. For deeper investigations on projects near the river — where soft clays and loose sands can extend well below 30 meters — we sometimes extend the array or pair MASW with a seismic refraction line to refine the bedrock depth interpretation without losing resolution in the shallow layers.
A measured VS30 of 260 m/s versus an assumed 180 m/s can move a site from Site Class E to D, and in Little Rock that difference can change the seismic base shear by a factor of two.
