This remote farmstead was one of the places where John Wesley, the founder of Methodism, preached his non-conformist doctrine in the 18th century. Every July it is still the scene of an obscure Methodist celebration known as the Love Feast. Instead of the usual communion wine and wafers, the congregation share fruitcake and water from a two-handled Loving Cup, to commemorate the non-conformist tradition.
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It’s strange to think that the lakes and forestry of the Derwent Dams, as they are known, are an entirely unnatural and man-made landscape. But nonetheless they are a popular playground for visitors to the Peak District National Park, especially from the neighbouring city of Sheffield. The reservoirs themselves are obviously an introduced feature, and the coniferous forestry plantations which surround them were planted because of a perceived need for water purity. It was thought that human development and grazing sheep might pollute the water flowing into the reservoirs so the trees were planted as a ‘natural’ filter.
The parallel Alport Dale, on the other hand, shows what the Upper Derwent used to look like before the water engineers cast their eyes on its water supply capabilities. And the amazing, spectacular landscape of Alport Castles shows the power of natural erosion in one of the Peak’s most remote and least visited valleys.
This is one of the geological and scenic highlights of the Peak District National Park. Alport Castles is said to be the largest landslip in Britain, but it is rarely visited because of its remoteness.
The Alport Valley is made up of weak Carboniferous shales (fine-grained rocks made of mud) overlain by harder Millstone Grit. The large cliff face we see here is the Birchin Hat escarpment. Alport Castles formed when the softer sandstones and shales of Birchin Hat slipped away from the rock-face. The Millstone Grit on the top broke up into blocks and tumbled down the valley side, creating a chaotic landscape of fallen boulders. With a little imagination, they can resemble castles – hence the name.
The Snake Pass, between the western arm of the Ladybower Reservoir at Ashopton and Glossop, is one of the shortest routes linking Sheffield and Manchester. It reaches a height of 1,680ft at Snake Summit. The road is well known from winter weather forecasts: it is one of the first roads to close in winter snows – and one of the last to reopen.
Despite what some people think, the pass takes its name from the serpent-headed coat of arms of the Dukes of Devonshire, and not from its winding nature. The Dukes of Devonshire and Norfolk, both prominent local landowners, contributed greatly towards the cost of the Sheffield to Glossop Turnpike road when it was constructed between 1818 and 1821, to a design by the Sheffield surveyor, William Fairbank.
The triple chain of the Howden, Derwent and Ladybower Reservoirs which flood the Upper Derwent Valley, represent the largest area of water in the Peak, and has been dubbed the Peak District’s Lake District.
The Derwent Dams were constructed by the Derwent Valley Water Board (now Severn-Trent) to supply fresh clean water to the fast-expanding industrial populations of Sheffield, Derby, Nottingham and Leicester.
The first two massive masonry dams constructed were the Howden and Derwent, between 1902 and 1916. During construction a temporary village, known as Tin Town because of its corrugated iron walls and roofs, housed the 1,000 or so navvies (labourers) and their families.
The larger Ladybower dam and reservoir followed in 1943, and took two years to finally fill! To accommodate the reservoirs, the villages of Derwent and Ashopton were demolished and their residents were re-housed at nearby Bamford. In times of drought, the foundations of some of the buildings can still be seen rising from the water.