NBCC 2015 Division B requires monitoring plans when cuts exceed 1.5 m in sensitive zones, and much of Pickering sits on glaciolacustrine clay with a high water table near the Duffins Creek corridor. The clay here is mapped as Halton Till overlying shale, with groundwater perched above the bedrock at depths that shift seasonally. Construction around Liverpool Road and the 407 extension has exposed these conditions repeatedly. For any shoring system, we combine automated total station readings with in-place inclinometers that feed data to the site engineer every four hours. A deep excavation design that ignores real pore pressure changes in this lacustrine soil can lose lateral support within a single storm cycle. Our role is instrument selection, threshold calibration, and continuous interpretation so the contractor can adjust tieback tension or bracing before wall displacement reaches alert levels. We also correlate bench marks to Lake Ontario datum because settlement here often propagates laterally for tens of metres beyond the cut face.
In Pickering's glaciolacustrine clay, lateral deformation propagates well beyond the cut face, so monitoring arrays must extend past the theoretical influence zone by at least 50 percent.
