The heavy clays deposited by the glacial Lake Algonquin define subsurface behavior in Sault Ste. Marie. Anyone breaking ground on the Precambrian fringe quickly discovers that what looks like stable terrain can hide compressible silt lenses twenty meters deep. The soil mechanics study we run here focuses on that contrast: the stiff till cap and the soft lacustrine sediment beneath it. A foundation designed for Windsor won't perform the same way on the north shore of the St. Marys River. Seasonal saturation cycles, freeze-thaw depth reaching two meters, and the proximity of the shield rock all demand a site-specific geotechnical profile. We process Shelby tube samples and remolded specimens to deliver shear strength parameters and consolidation curves that the structural engineer can use directly in the NBCC load and resistance factor design.
Varved clay from the Sault plain can lose half its shear strength when remolded — sensitivity ratios above 8 are common.
