Rock that can take water, and rock that can't
The county has a few ground types that tend to drain. The Magnesian Limestone ridge around Bolsover and Whitwell is permeable, and so are the sand and gravel terraces along the Trent, the Dove and the lower Derwent. The Carboniferous limestone of the White Peak passes water readily too, though its open fissures mean the engineer has to think about where the water goes once it leaves the crates.
Elsewhere the picture is poorer. The Mercia Mudstone around Derby, the Coal Measures of the north-east and the shales of the Dark Peak usually give slow results. On those, a soakaway that can't empty between storms is worse than none, and attenuation is the honest answer.


