In Adelaide, you can dig in two spots fifty metres apart and find completely different soil profiles—that’s just how the local geology works. We’ve opened test pits where one corner of the site hit calcrete at 1.2 m while the other went through 2 m of uncontrolled fill from the 1960s. An exploratory test pit gives you that direct visual record, no guesswork. We log the stratigraphy, take block samples for lab testing, and check for moisture conditions that react badly with the city’s reactive clay belts. When the pit hits weathered siltstone, we often cross-check findings with an SPT drilling log to confirm refusal depth, or pair it with a grain size analysis to classify the fine fraction that causes volume change in the Adelaide Hills.
A single carefully logged test pit in Adelaide’s reactive clay zone can save you from footing movement claims that would surface three summers later.
