Kamloops grew rapidly after the Canadian Pacific Railway pushed through the Thompson Valley in the 1880s, and that growth pushed development onto increasingly steep terrain. The city sits at the confluence of the North and South Thompson Rivers, surrounded by benchlands and deeply incised gullies carved into glacial lake sediments. Every excavation, road widening, or hillside foundation in this city interacts with a complex geological history. We run slope stability analysis here with a clear focus: determine the factor of safety under both static and seismic loading, identify failure surfaces before they become problems, and give contractors and developers numbers they can trust. When a site sits on silt-rich glaciolacustrine deposits that lose strength when saturated, we often recommend pairing the analysis with a CPT investigation to map continuous stratigraphy and identify weak layers that traditional boreholes might miss.
A slope that stands today may fail tomorrow when pore pressures rise; we quantify that threshold so you don't discover it by accident.
