We ran a resistivity line last autumn across a proposed warehouse site near the A420. The client needed to know bedrock depth before piling design. Swindon's geology isn't uniform. The southern edge sits on coral-rich limestone of the White Horse country, while the north transitions into Oxford Clay. That contrast creates a perfect scenario for electrical methods. We set up a Schlumberger array with a maximum AB/2 of 150 metres. The data showed a clear resistive layer at 8 metres depth. Correlating that with a single CPT test confirmed it was the Cornbrash formation. The survey took four hours. The report was delivered the next day. No drilling damage, no traffic disruption, no guesswork. That's the power of a well-executed VES survey.
A VES survey in Swindon's Oxford Clay can map the weathered-to-competent transition without a single borehole. That saves weeks in the site investigation programme.



