© Mapbox · © OpenStreetMap contributors · Boundary data © Historic England (NHLE)
Scots' Dike is a linear earthwork located in Cumberland, England, traditionally attributed to the medieval period as a boundary feature marking the frontier between England and Scotland. The monument takes the form of a substantial bank and ditch running across the landscape, characteristic of medieval defensive and demarcation works of the Anglo-Scottish borderlands. Its exact dating and original purpose remain subjects of scholarly discussion, though it is documented as a significant landscape feature in the borderland region. The dike represents the physical manifestation of political boundaries that were contested and negotiated throughout the medieval period in this strategically important area.
Scots' Dike is a scheduled monument protected by Historic England under reference 1016860. View the official record →
Scots' Dike is a linear earthwork located in Cumberland, England, traditionally attributed to the medieval period as a boundary feature marking the frontier between England and Scotland. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1016860.
Scots' Dike 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 1016860.
Several scheduled monuments lie within 10 km, including Woodslee,burial mound 250m SW of (1.6 km), Liddel Strength motte and bailey castle and fortified tower house (2.8 km), Scots' Dike, boundary earthwork, Scotsdike Plantation (3.2 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Scots' Dike'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.
Scots' Dike stands on Triassic Rocks (Undifferentiated), bedrock that formed in the Triassic. The rock here is sandstone and conglomerate, interbedded.