Ground that changes across the county
The sandstones and pebble beds that form Cannock Chase drain quickly, and plots on them can often return roof water straight to the ground. The Trent and Dove valleys have sand and gravel terraces that drain too, though groundwater in them can sit close to the surface. In the north, the Coal Measures around Stoke-on-Trent and Kidsgrove, and the mudstone across much of the middle of the county, hold water and usually rule infiltration out.
Limestone and gritstone in the Moorlands raise their own questions for the engineer. None of this is ours to judge on site: the soakaway is sized from percolation results and placed by your designer, and we install to that drawing.



