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Section of linear boundary dyke on Millington Lings 625m north east of High Callis Wold is a prehistoric earthwork monument located on the Yorkshire Wolds. The dyke represents a substantial linear boundary structure characteristic of Iron Age or Late Bronze Age land division and territorial demarcation in this region. The monument survives as a visible earthwork feature within the landscape of Millington Lings, forming part of the broader system of ancient field boundaries and defensive works documented across the Yorkshire Wolds. Such dykes functioned to demarcate property or territorial boundaries and reflect the organised agricultural and social structures of Iron Age communities in northern England.
Section of linear boundary dyke on Millington Lings 625m north east of High Callis Wold is a scheduled monument protected by Historic England under reference 1015574. View the official record →
Section of linear boundary dyke on Millington Lings 625m north east of High Callis Wold is a prehistoric earthwork monument located on the Yorkshire Wolds. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1015574.
Section of linear boundary dyke on Millington Lings 625m north east of High Callis 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 1015574.
Several scheduled monuments lie within 10 km, including Cross base and shaft and cross base at St Margaret's Church (4.5 km), Round barrow 520m S of Warren Farm (4.9 km), Deepdale cross ridge dyke (5 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Section of linear boundary dyke on Millington Lings 625m north east of High Callis 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 linear boundary dyke on Millington Lings 625m north east of High Callis Wold stands on White Chalk Subgroup, bedrock that formed in the Maastrichtian. The rock here is chalk.