North Bay's development along the Canadian Shield margin created a unique geotechnical fingerprint—where the retreat of the Laurentide Ice Sheet dumped a chaotic mix of glacial till, varved silts, and pockets of glaciolacustrine clay across what is now the city's residential and industrial zones. Highway 11/17 corridors cut straight through these deposits, and anyone who's drilled near Trout Lake knows the material changes every few meters. A standard grain size analysis combining mechanical sieving with hydrometer sedimentation reads this stratigraphy in precise percentages—gravel, sand, silt, and clay fractions that dictate everything from frost susceptibility under Nipissing District winters to permeability assumptions for stormwater infiltration. Our Ontario-accredited lab runs the full ASTM D422/D7928 suite, delivering gradation curves that engineers rely on for seismic microzonation assessments and foundation drain design in the city's silty-clay neighborhoods.
A single hydrometer reading can reclassify a soil from silty sand to sandy silt—and that distinction changes the entire drainage design for a North Bay foundation.
