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Section of linear boundary dyke in and extending to the north west of Farclose Plantation towards Waterman Hole is a linear earthwork of probable Iron Age or Romano-British date located in Yorkshire, England. The dyke survives as a substantial bank and ditch arrangement, characteristic of boundary works constructed to demarcate territorial divisions or defensive perimeters during the prehistoric and Roman periods. Such linear earthworks served important functions in managing land use and controlling movement across the landscape, reflecting the social and political organisation of their time. The monument is recorded on the National Heritage List for England under entry number 1015559.
Section of linear boundary dyke in and extending to the north west of Farclose Plantation towards Waterman Hole is a scheduled monument protected by Historic England under reference 1015559. View the official record →
Section of linear boundary dyke in and extending to the north west of Farclose Plantation towards Waterman Hole is a linear earthwork of probable Iron Age or Romano-British date located in Yorkshire, England. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1015559.
Section of linear boundary dyke in and extending to the north west of Farclose Plantation towards Waterman Hole 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 1015559.
Several scheduled monuments lie within 10 km, including Round barrow 600m west of Newcote Farm (5.9 km), Site of Warter Augustinian Priory (6.1 km), Round barrow 915m north east of Dalton Gates Farm (6.5 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Section of linear boundary dyke in and extending to the north west of Farclose Plantation towards Waterman Hole'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 linear boundary dyke in and extending to the north west of Farclose Plantation towards Waterman Hole stands on White Chalk Subgroup, bedrock that formed in the Maastrichtian. The rock here is chalk.