Applying the National Building Code of Canada (NBCC 2020) in North Bay is not a generic checkbox exercise—especially on the glaciofluvial sands that blanket the Nipissing paleo-plain. A standard borehole log with blow counts won't tell you whether those saturated fine sands at 4 m depth will lose all strength during a 1-in-475-year seismic event. We run a cyclic stress ratio (CSR) evaluation against the normalized SPT or CPT resistance, because the Widdifield Formation deposits here often plot in the ‘suspect’ zone on a Seed & Idriss boundary curve. For projects within the Nipissing District where the water table sits less than 2 m below grade, we pair the CPT test with laboratory cyclic triaxial to validate the triggering analysis, ensuring your geotechnical report withstands review by the City of North Bay building department. The site-specific ground motion we input comes from the Geological Survey of Canada’s 5th Generation Seismic Hazard Model, not a blanket zone factor.
Post-liquefaction volumetric strain in North Bay's Trout Lake outwash can exceed 3% at CSR values above 0.25—enough to tilt a shallow footing beyond serviceability.
