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Sections of linear boundary dyke in Frendal Dale, Tun Dale, and Great Plantation, between Millington and Huggate Wolds, is a prehistoric or early historic earthwork comprising substantial linear banks and ditches that traverse the Yorkshire Wolds landscape. The dyke represents a boundary or defensive structure, with surviving sections visible across three distinct locations within the rolling downland terrain between these two chalk ridge features. The monument is scheduled as an ancient monument in recognition of its significance as evidence of land division or territorial demarcation during the prehistoric or early medieval period. The dykes survive as substantial buried and surface features that contribute to understanding patterns of early landscape organization and land use across the Wolds region.
Sections of linear boundary dyke in Frendal Dale, Tun Dale, and Great Plantation, between Millington and Huggate Wolds is a scheduled monument protected by Historic England under reference 1015561. View the official record →
Sections of linear boundary dyke in Frendal Dale, Tun Dale, and Great Plantation, between Millington and Huggate Wolds, is a prehistoric or early historic earthwork comprising substantial linear banks and ditches that traverse the Yorkshire Wolds landscape. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1015561.
Sections of linear boundary dyke in Frendal Dale, Tun Dale, and Great Plantation, between Millington and Huggate Wolds 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 1015561.
Several scheduled monuments lie within 10 km, including Round barrow 600m west of Newcote Farm (5 km), Site of Warter Augustinian Priory (5.5 km), Ousethorpe medieval settlement, moat and mill 310m south of Ousethorpe Farm (6.1 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Sections of linear boundary dyke in Frendal Dale, Tun Dale, and Great Plantation, between Millington and Huggate Wolds'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.
Sections of linear boundary dyke in Frendal Dale, Tun Dale, and Great Plantation, between Millington and Huggate Wolds stands on White Chalk Subgroup, bedrock that formed in the Maastrichtian. The rock here is chalk.