A foundation on the sandy till near Frenchman's Bay has almost nothing in common with one set into the compact silts of the Duffin Heights moraine—even though both sit inside Pickering's boundaries. The difference isn't visible from a backhoe trench, but it shows up immediately in a shear wave velocity profile. When we run a MASW survey, the array of geophones picks up how fast energy moves through the upper 30 metres, giving us the VS30 value that defines seismic site class. That single number drives the seismic design loads in the National Building Code, and getting it wrong means either an overbuilt foundation or a dangerously under-designed one. In Pickering's post-glacial landscape, where till ridges meet lake-bottom clays, we often pair the surface wave data with a few SPT boreholes to tie the velocity model to actual soil stratigraphy, especially when the client needs a Class C or D determination for a mid-rise residential block.
VS30 is not a box-ticking exercise—in Pickering's glacial terrain, a default site class assumption can misrepresent seismic demand by a full code level.
