Why Derbyshire ponds need a liner
Derbyshire's ground changes quickly from north to south, and very little of it holds water reliably on its own. The White Peak is Carboniferous limestone: jointed, fissured rock that water drains straight down through. That's why the old dew ponds and meres on the limestone plateau were always puddled with clay. The Dark Peak to the north is gritstone and shale, with thin acid soils and springs that come and go with the seasons.
Further east, the coalfield around Chesterfield and the Erewash valley has mixed ground and old workings, and the Trent and Dove valleys carry sand and gravel terraces. Gravel drains freely, and clay that looks tight in a trial pit can crack open in a dry summer. On every one of those grounds the safe answer is the same: a membrane welded in place over a cushioning underlay.


