A six-story mixed-use job off Mercury Boulevard hit limestone pinnacles nobody expected. The borings missed them. We brought in the seismic spread, ran a refraction profile along the building footprint, and mapped the rock surface within 0.5 meters. Hampton's geology is like that—coastal plain sediments draped over a weathered basement that doesn't always cooperate with a drill rig. Seismic tomography gives us the continuous image that spot borings can't provide. When you need to know where competent bearing lies, or you're chasing the top of the Yorktown Formation, the MASW survey complements the P-wave data with a shear-wave velocity column that feeds straight into the IBC site classification table. The city's 137,000 residents live atop a subsurface that demands this kind of resolution.
A single boring gives you 8 inches of information. A seismic line gives you 200 feet of continuous subsurface—that's the difference when site class boundaries shift by 15 meters.



