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Section of single linear boundary dyke in Horse Dale, 550m north west of Glebe Farm is a linear earthwork in North Yorkshire comprising a single bank and ditch. The dyke is scheduled as an ancient monument and is registered on the National Heritage List for England under entry 1015565. Such linear boundary features in the Yorkshire landscape typically date to the Iron Age or Romano-British period, serving as territorial divisions or field boundaries within the agricultural landscape. The surviving section preserves evidence of past land management practices and territorial organisation in this part of Yorkshire.
Section of single linear boundary dyke in Horse Dale, 550m north west of Glebe Farm is a scheduled monument protected by Historic England under reference 1015565. View the official record →
Section of single linear boundary dyke in Horse Dale, 550m north west of Glebe Farm is a linear earthwork in North Yorkshire comprising a single bank and ditch. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1015565.
Section of single linear boundary dyke in Horse Dale, 550m north west of Glebe 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 1015565.
Several scheduled monuments lie within 10 km, including Round barrow 915m north east of Dalton Gates Farm (5.7 km), Round barrow 930m north east of Dalton Gates Farm (5.8 km), Two round barrows 820m north east of Dalton Gates Farm (5.8 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Section of single linear boundary dyke in Horse Dale, 550m north west of Glebe 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 single linear boundary dyke in Horse Dale, 550m north west of Glebe Farm stands on White Chalk Subgroup, bedrock that formed in the Maastrichtian. The rock here is chalk.