Wade's Causeway

Wade’s Causeway is a raised stone track that runs across Wheeldale Moor in the North York Moors. Its origins are debated: mid-20th-century digs dated it to the Roman period, yet 21st-century studies suggest it could be Neolithic. The best-preserved stretch is just over a mile long and protected as a scheduled monument. Local folklore once credited its construction to Wade, a giant from Germanic myth. The moorland setting remains largely unchanged since the Bronze Age, with patches of sand and gravel over sandstone and limestone. Experts agree the embankment was built to keep the surface dry. Archaeologist David E Johnston notes small drainage culverts cut through the structure to carry off becks that often flood the boggy ground. Nikolaus Pevsner and Richard Muir believe a gravel layer once topped the stone flags, later lost to weathering or human removal. Nineteenth-century writers such as Thomas Codrington described a double layer of stones and gravel in 1817, and traces of smaller pebbles were still visible in the 1960s. The visible section shows closely fitted sandstone slabs averaging 45 centimetres square, with some as broad as 1.5 metres. The clearly seen stretch runs north-northeasterly for about 1.2 miles at roughly 200 metres above sea level. Its straight alignments occasionally shift direction in ways not forced by the landscape. In 1855 overgrown fragments were reported near Morley Cross and Castle Hill, but no other parts of the conjectured 25-mile route survive visibly today. Aerial traces hint at a possible continuation past Hazle Head towards the Roman fort at Lease Rigg, though this remains unproven.