Sandstone in the north, clay in the vales
Worcestershire's ground divides more sharply than most counties. A band of Triassic sandstone runs from the Lickey Hills down through Bromsgrove and out towards Kidderminster, Hartlebury and Stourport, and roof water on that ground can often be returned to the rock a few metres from the downpipe. South and east of Worcester, the red Mercia Mudstone and the Lias clays of the Vale of Evesham keep water at the surface, and a soakaway dug into them tends to fill and stay full.
The river terraces of the Severn and the Avon make a third case: gravels that drain freely but sit over groundwater that can rise near the surface in a wet winter. Which of these a plot is on, and whether crates suit it, is settled by percolation results and your engineer's design rather than by us. We build what those numbers support.



