Swaledale occupies the long, sinuous valley carved by the River Swale on its 45-kilometre descent from Nine Standards Rigg (662 m) on the Pennine watershed to Richmond in lower Teesdale. The dale narrows between rough gritstone scarps near Keld, broadens to a patchwork of hay-meadows around Muker and Gunnerside, then opens into a tree-fringed flood-plain west of Reeth before the river cuts through the Carboniferous escarpment to meet the Vale of Mowbray.
Period: Any Period
Aug 04
Guide: Parliamentary-walls and the Northern Enclosures
Between the mid-18th and late-19th centuries the British Parliament passed almost 5,000 local “Inclosure Acts.” Each Act authorised a team of appointed commissioners to survey one specific township or parish, divide its open-field strips, common pastures, and “wastes” into new, privately owned parcels, and lay out straight roads and boundary walls or hedges. The commissioners issued a legal award map and schedule that became the new title deeds.
Bishopdale
Bishopdale lies within the northern limb of the Askrigg Block, its underlying bedrock dominated by Carboniferous limestones with intermittent shales and sandstones of the Yoredale Series. The Great Scar Limestone, a thick, massive unit formed around 330 million years ago in a shallow tropical sea, underpins the dale’s steeper scarps and cliff lines, while the thinner-bedded limestones and intervening mudstones of the Yoredale Group create the characteristic terraced flanks on which many of Bishopdale’s field systems are laid out

