Melbourne sits on a mix of Quaternary basalts in the west, Silurian mudstones in the east, and the notorious Coode Island Silt beneath the CBD. That soft silty clay, up to 40 m deep in places, requires careful measurement of drained and undrained strength before any deep excavation. Our direct shear test isolates the failure plane along a controlled horizontal surface, giving you cohesion and friction angle for slope stability or footing design. We run the test under consolidated-drained or consolidated-undrained conditions, matching the in-situ stress path of your site. For shallow foundations on the Brighton Sandy Loam, we combine the direct shear result with a plate load test to confirm bearing capacity in the field.

Peak friction angles on Melbourne's Silurian mudstones range from 38° to 44°, but residual values can drop below 25° on pre-existing slickensides.