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A section of linear boundary dyke 160m west of High Callis Wold Farm is a prehistoric or early historic earthwork located in Yorkshire. The dyke represents an example of linear defensive or demarcating structures characteristic of Iron Age or Romano-British settlement patterns in northern England. The monument survives as a substantial bank and ditch formation that would have functioned as a territorial boundary or defensive feature for a contemporary settlement. Such linear dykes are typically associated with estate management and land division during periods of intensified agricultural activity and social organisation in the later Iron Age or Romano-British periods.
Section of linear boundary dyke 160m west of High Callis Wold Farm is a scheduled monument protected by Historic England under reference 1015609. View the official record →
A section of linear boundary dyke 160m west of High Callis Wold Farm is a prehistoric or early historic earthwork located in Yorkshire. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1015609.
Section of linear boundary dyke 160m west of High Callis Wold Farm 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 1015609.
Several scheduled monuments lie within 10 km, including Round barrow 100m SW of Cobdale Farm (3.7 km), Section of linear boundary dyke between Sylvan Dale and Warren Farm, north west of Coldwold Farm (3.8 km), Cross base and shaft and cross base at St Margaret's Church (4 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Section of linear boundary dyke 160m west of High Callis Wold Farm'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 160m west of High Callis Wold Farm stands on White Chalk Subgroup, bedrock that formed in the Maastrichtian. The rock here is chalk.