Ottawa sits at roughly 70 meters above sea level, but the subsurface tells a more complicated story. The city rests on a mix of glacial till and the infamous Leda clay, a sensitive marine deposit that has triggered retrogressive landslides in the region. When you cut into a slope along the Rideau River or plan an embankment in Kanata, the safety factor is not a guess—it is a calculation backed by effective stress parameters. A triaxial test program gives us the drained and undrained shear strength we need to model failure surfaces accurately, while grain-size analysis confirms whether the matrix is truly a sensitive silt-clay or something more stable. Every project in the Ottawa Valley has to account for the Champlain Sea deposits; ignoring them is a gamble no engineer will take.
A stability number under 0.15 in Leda clay means you are managing a potential retrogressive landslide, not just a surface slough.



