Excavating in Centretown with its urban fill is a different world from cutting into the sensitive Leda clay deposits south of Hunt Club. Ottawa’s geology shifts dramatically within a few kilometers, and a monitoring plan that works for a sandy till in Kanata can fail completely in the Champlain Sea silts of Vanier. Our team deploys instrument arrays that match the specific stratigraphy of each site, tracking lateral movement, groundwater fluctuation, and vibration transmission. Before installing the shoring, we often complement the subsurface profile with CPT soundings to identify thin drainage layers that trigger instability, and we verify the bedrock refusal depth with seismic refraction to ensure the monitoring anchors have competent grip. The goal is to detect deformation patterns before they become structural problems for the excavation or the adjacent heritage buildings.
A 4 mm/day creep in Leda clay at 11 m depth won't show on the surface—but it will fail a shoring wall within a week if unaddressed.



