The Severn Vale's geology shapes every foundation decision in Cheltenham. Beneath the Regency terraces, the Charmouth Mudstone Formation — part of the Lower Lias — weathers to a stiff, fissured clay that swells seasonally with the Cotswold rainfall. Across the town centre and towards the racecourse, pockets of Cheltenham Sand and Gravel introduce a different challenge: loose granular lenses at shallow depth that compact unpredictably under load. A CPT test across a site near Pittville Park will often show a cone resistance drop from 8 MPa in the clay to below 2 MPa in these gravel seams — exactly the contrast that vibrocompaction design has to reconcile. Our team models the interaction between the Lias formation and these alluvial channels to specify vibrator spacing, frequency, and dwell time that densify the loose zones without remoulding the surrounding clay. We work to BS EN 1997-1:2004, applying Design Approach 1 for ultimate limit state verification, because Cheltenham's mixed stratigraphy demands both strength and serviceability checks that a single partial factor set cannot capture.
Post-treatment CPT in Cheltenham's gravel lenses should show a cone resistance increase of at least 2.5 times the pre-treatment value to confirm the design relative density.



