The Willamette River has shaped Eugene’s subsurface for millennia, leaving behind thick deposits of loose alluvial silts and sands that challenge any foundation. With the city's proximity to the Cascadia Subduction Zone, these granular soils are susceptible to settlement and liquefaction during a seismic event. Vibrocompaction design in Eugene must account for variable groundwater tables and the transition zones between valley fill and older terrace gravels. Our approach integrates site-specific CPT testing to map target layers and liquefaction analysis per NCEER protocols, ensuring the Improvement strategy fits the depositional complexity unique to this part of Lane County.
Post-treatment verification in Eugene’s river deposits typically shows a 30 to 60 percent increase in cone tip resistance within the treated zone.
