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Section of double linear boundary dyke west of Far Out Field, Millington Wold is a prehistoric earthwork consisting of two parallel linear ditches situated on the Yorkshire Wolds. The dyke is scheduled as an ancient monument of regional archaeological significance, forming part of the landscape management systems characteristic of Bronze Age or Iron Age settlement patterns in the region. The double linear form suggests a boundary marker of considerable importance, possibly defining territorial limits or controlling livestock movement across the Wolds. The monument remains visible as an earthwork feature and contributes to understanding the prehistoric organisation of this upland landscape.
Section of double linear boundary dyke west of Far Out Field, Millington Wold is a scheduled monument protected by Historic England under reference 1015572. View the official record →
Section of double linear boundary dyke west of Far Out Field, Millington Wold is a prehistoric earthwork consisting of two parallel linear ditches situated on the Yorkshire Wolds. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1015572.
Section of double linear boundary dyke west of Far Out Field, Millington Wold 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 1015572.
Several scheduled monuments lie within 10 km, including Round barrow 520m S of Warren Farm (4.3 km), Deepdale cross ridge dyke (4.3 km), Round barrow 600m west of Newcote Farm (4.8 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Section of double linear boundary dyke west of Far Out Field, Millington Wold'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 double linear boundary dyke west of Far Out Field, Millington Wold stands on White Chalk Subgroup, bedrock that formed in the Maastrichtian. The rock here is chalk.