In Celbridge we keep seeing the same pattern. A site looks fine on the surface but the ground underneath tells a different story. Much of the town sits on glacial till overlying Carboniferous limestone. The till is dense. It's stony. It varies over short distances. Standard drilling struggles here. The CPT pushes a cone through these deposits and records resistance continuously. You get a sharp profile of where the till tightens up and where the limestone bedrock begins. For engineers working along the R403 or near Castletown House, this data is gold. We run the test with a 20-tonne rig and a 15 cm² cone. The friction sleeve picks up subtle changes in clay content. The pore pressure transducer flags silt lenses before they become a problem during excavation. When the Liffey is high after winter rain, we often combine this with an in-situ permeability assessment to check how groundwater moves through the upper drift.
In Celbridge's mixed glacial deposits, a single CPT sounding often reveals more about stratigraphy than three boreholes combined.
