Sydney's coastal geology creates a complex mix of Hawkesbury Sandstone, shale, and deep alluvial deposits along the Parramatta River. The humid subtropical climate and historic land reclamation in areas like Pyrmont and Barangaroo mean fill layers can hide abrupt changes in density. In our experience, the SPT is the most direct way to catch these transitions before they cause settlement issues. By driving a split-spoon sampler with a 63.5 kg hammer, the test delivers N-values that correlate to relative density and shear strength. For sites near the harbour foreshore, combining SPT data with a georradar GPR survey helps map buried utilities and old seawalls before drilling begins.

A single SPT borehole can reveal an abrupt transition from loose fill to deep sandstone, saving weeks of redesign later.