The biggest mistake we see on Gloucester sites is assuming the geology is uniform because the ground looks flat. The Severn Vale hides a patchwork of river terrace gravels, alluvial silts, and the underlying Lias Clay. Digging a borehole in the wrong spot misses a lens of soft peat that will cause differential settlement later. Our team runs exploratory test pits across the city to expose the real soil sequence. A test pit lets you see the transition between fill and natural ground with your own eyes, while a grain size analysis of sampled material confirms whether that sandy layer is well-graded or gap-graded. For sites near the River Severn or the Gloucester and Sharpness Canal, we often combine pit logging with in-situ permeability testing to check how fast water moves through the terrace gravels.
A single exploratory test pit reveals more about ground variability than a desk study ever can. In Gloucester, the difference between gravel and clay can be a matter of metres.
