St. Catharines grew along the old Welland Canals, layered over glaciolacustrine silts and sands deposited by Lake Iroquois. That history matters when you are dealing with seismic risk. The downtown core and north-end industrial areas sit on saturated granular soils that, under the right earthquake loading, can lose strength entirely. We look at liquefaction potential not as a generic checkbox, but as a local question tied directly to the stratigraphy of the Niagara Escarpment benchlands. When a site investigation reveals loose sands below the water table, typically within the upper 15 metres, the next logical step is pairing the field data with a CPT test to get a continuous profile of tip resistance and sleeve friction, which feeds directly into the cyclic stress ratio calculations required by NBCC 2020 seismic provisions.
A saturated fine sand in St. Catharines with SPT N-values under 10 in the upper 5 metres will nearly always flag a liquefaction review under NBCC seismic hazard values.
