Vancouver sits on a complex geological mix: deep marine silts and clays in the Fraser River delta, compact glacial till on the uplands, and localized peat deposits in areas like Richmond. When the 2015 M4.8 earthquake shook the Strait of Georgia, it reminded engineers that fine-grained soils behave very differently under loading depending on their moisture content. The Atterberg limits test, run to ASTM D4318-17e1 in our accredited lab, determines the liquid limit, plastic limit, and plasticity index — numbers that dictate how a clay will consolidate, swell, or lose strength. For projects near False Creek or along the Burrard Inlet, where soft post-glacial silts dominate, these limits feed directly into settlement calculations and slope stability assessments required by the City’s building bylaw.
The plasticity index tells you more about a Vancouver clay's behavior under cyclic loading than the SPT blow count alone.
