Sarnia sits roughly 190 meters above sea level, perched on the edge of the St. Clair River. That elevation looks modest until you factor in the riverbank erosion rates that have shaped this city since the 1850s. For any excavation deeper than 1.2 meters in Sarnia’s glaciolacustrine clays, the stability window tightens fast. We run slope stability analysis that maps the failure envelope before a bucket hits the ground. The approach integrates Sarnia’s known stratigraphy—stiff clay till overlying Kettle Point shale—with pore pressure data collected on site. The result is a factor of safety you can defend to the municipality and the consulting engineer. When the stratigraphy turns complex, we often pair the analysis with a CPT test to capture continuous soil behavior without gaps, or with test pits when the upper two meters need visual confirmation of fill and organics.
In Sarnia clay, the factor of safety drops 15% within 72 hours of cutting a vertical face—timing the analysis matters as much as the method.
