In Ottawa, the difference between a routine footing and a structural headache often comes down to what lies beneath the topsoil. The city sits on a complex glacial legacy—Champlain Sea sediments, better known as Leda clay, dominate the eastern and central corridors, while glacial till and bedrock outcrops control the western neighborhoods. Anyone breaking ground near the Greenbelt or along the Rideau River quickly learns that soil stiffness can shift within a single building footprint. Our team runs field verification and laboratory strength testing so that shallow foundation design matches the actual stratigraphy, not just the regional map. This approach avoids over-excavation and keeps bearing pressures within the allowable limits set by the Ontario Building Code, referencing NBCC 2015 Part 4. Before finalizing a footing width, we often recommend a complementary CPT test to profile soft clay lenses that standard boreholes might miss.
Ottawa’s 1.8-meter frost line isn’t a suggestion—ignoring it in shallow foundation design turns a March thaw into a differential movement claim.



