Dufton: Village History and Landscape

Dufton combines a historic village layout with distinctive geological formations and two routes with different focuses. The village lies just inside the boundary of the North Pennines Area of Outstanding Natural Beauty. The Pennine Way and Route 68 of the National Cycle Network pass through Dufton. These connections offer different themes to explore when planning your trip, from village history to walking and cycling.

Village Layout and Historic Buildings

A lime tree avenue runs through the centre of the rectangular village green. Much of the village was designated a conservation area on 27 June 2005. The surviving buildings also offer a glimpse of its earlier architectural history: almost a third of the oldest surviving buildings date from the 17th and early 18th centuries. Dufton Hall dates back at least to the 17th century; the building may have originated as early as the 16th century. Its date of origin therefore remains deliberately open. The Church of St Cuthbert is a medieval church, rebuilt in 1784.

The history of the village extends beyond these buildings. Old Dufton refers to the remains of a Romano-British settlement about three-quarters of a mile above the present village. Lead mining represents another period in its history: lead mining and smelting employed many of Dufton’s residents in the 19th century. This allows the different periods to be distinguished—from the early history of settlement, through medieval and early modern buildings, to the local history of mining.

Geology and Landscape

The landscape around Dufton offers several distinct geological features. The cliffs at High Cup Nick are made of dark, hard dolerite. High Cup Gill is a classic U-shaped valley, formed by ice and meltwater. Dufton Pike, meanwhile, is made of volcanic material. These details describe different characteristics: the rock in the cliffs, the shape and formation of a valley, and the composition of a hill.

The name “Helm Wind” is also part of the local landscape: Dufton lies at the centre of the area affected by this natural phenomenon. Together with its geological features, this creates a landscape that cannot be reduced to a single landform or type of rock.

Routes and Nature

The Pennine Way is a long-distance walking trail that passes through Dufton. Route 68 of the National Cycle Network also runs through the village. The two routes appeal to different travel interests: the Pennine Way is a long-distance walking trail, while Route 68 is a cycling route. If you are planning a ride on Route 68, check local route conditions in advance, as they can change.

Dufton Ghyll Wood is one of the few remaining north-western habitats of the native red squirrel. Dufton Gill is a semi-natural ancient woodland owned and managed by the Woodland Trust. St Bees Sandstone is exposed in the old quarries at Dufton Ghyll. These natural and geological features add questions of native wildlife, woodland landscape and regional geology to the history of the buildings and village.

Dufton offers several different ways to shape the focus of your trip: explore the village layout and its historic buildings, the Romano-British settlement remains, the 19th-century mining history, or the geological formations around High Cup Nick, High Cup Gill and Dufton Pike. If you are more interested in nature, you can also explore the importance of Dufton Ghyll Wood for the native red squirrel and the ancient woodland of Dufton Gill.

Discover more destinations: Alston, Broughton, Great Clifton, Sedbergh, Cartmel, Ireby, Tebay, Mungrisdale.

For the regional travel overview: Cumbria.