Under Part 4 of the Ontario Building Code (OBC) and the National Building Code of Canada (NBCC 2020), seismic site classification is mandatory for most structures, and in Pickering the geology makes liquefaction screening non-negotiable. The city sits above the Queenston Shale but its surface is draped with glaciolacustrine silts, sand lenses, and recent alluvial deposits along the Rouge River and Petticoat Creek corridors. These loose water-saturated granular layers, when subjected to the ground accelerations expected in a moderate to large earthquake originating from the western Lake Ontario seismic zone, can lose strength abruptly. Our field practice in Pickering involves running SPT-based liquefaction triggering analyses (Youd et al. 2001, and updated Boulanger & Idriss 2014 procedures) followed by post-triggering settlement and lateral spreading displacement estimates. The MASW seismic survey is often deployed first to map Vs profiles and identify soft zones without extensive drilling, and when refusal depths are uncertain we add CPT testing for continuous tip resistance and pore pressure data.
In Pickering, the difference between a code-minimum screening and a site-specific CRR curve from cyclic triaxial can mean the difference between stone columns and a conventional raft.
