© Mapbox · © OpenStreetMap contributors · Boundary data © Historic England (NHLE)
The Scots Dyke is a linear earthwork running through the moorland landscape east of Langdale Rush in Yorkshire. This substantial boundary bank, which survives as a prominent ridge in the terrain, dates from the medieval period and served as a territorial or defensive demarcation. The dyke represents an important example of the linear earthworks constructed across northern England during the medieval centuries, reflecting patterns of land management and administrative control characteristic of that era. Its precise original function—whether primarily defensive, administrative, or ceremonial in nature—remains a subject of archaeological interpretation, though its substantial surviving form testifies to the significance with which it was constructed and maintained.
Section of Scots Dyke linear boundary east of Langdale Rush is a scheduled monument protected by Historic England under reference 1014240. View the official record →
The Scots Dyke is a linear earthwork running through the moorland landscape east of Langdale Rush in Yorkshire. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1014240.
Section of Scots Dyke linear boundary east of Langdale Rush is a Scheduled Ancient Monument, legally protected by Historic England (NHLE) — the body responsible for designating and safeguarding heritage sites in England. The official designation reference is 1014240.
Several scheduled monuments lie within 10 km, including Section of Scots Dyke linear boundary and portion of field system 100m east of Whitefields Farm (8 km), Uckerby medieval village and open field system (8.6 km), Section of Scots Dyke linear boundary 75m south west of Sandford House (8.7 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Section of Scots Dyke linear boundary east of Langdale Rush's history, each drawn from the record and mapped to the exact spot:
Every location is different. Not every section appears for every place, only what the historical record actually holds turns up in a report.
Section of Scots Dyke linear boundary east of Langdale Rush stands on Yoredale Group, bedrock that formed in the Bashkirian. The rock here is limestone, sandstone, siltstone and mudstone.