In Swindon, the geological transition from the soft, weathered Kimmeridge Clay in the north and west to the stronger Cornbrash limestone and Forest Marble formations underpinning the town centre creates a highly variable geotechnical profile that standard desk studies often fail to capture. We regularly see projects where initial assumptions about bearing capacity are overturned once the split-spoon sampler hits the dense gravels of the ancient River Ray terraces, revealing N-values that jump from single digits to over 50 blows in less than a metre. The Standard Penetration Test remains the most direct method for quantifying this vertical heterogeneity, and when executed under BS 5930:2015+A1:2020 procedures, the resulting N60 values provide a reliable basis for both shallow and deep foundation design. Our technical team has correlated hundreds of SPT profiles across Swindon, from the swelling clays near Coate Water to the limestone brash in Old Town, allowing us to contextualize raw blow counts against local depositional history rather than relying solely on generic empirical correlations. For a complete stratigraphic picture, we often integrate our SPT data with continuous CPT soundings when the upper clay layers require a more refined assessment of undrained shear strength before selecting a piling strategy.
An SPT N-value of 4 in Swindon’s alluvial clays demands a completely different foundation solution than an N-value of 35 in the Cornbrash, even when the two strata are separated by only two metres of vertical depth.



