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Linear boundary earthwork 370m east of Oscar Park Farm is a prehistoric or early historic linear earthwork located in Yorkshire, England. The monument comprises a substantial linear bank and ditch feature characteristic of boundary systems that may date to the Iron Age or Romano-British period, though its precise chronology remains uncertain without excavation. Such linear earthworks commonly served to demarcate territorial boundaries, control livestock movement, or define land divisions within ancient landscapes. The feature is scheduled as an ancient monument and remains of archaeological interest for understanding the settlement patterns and land use of north Yorkshire during antiquity.
Linear boundary earthwork 370m east of Oscar Park Farm is a scheduled monument protected by Historic England under reference 1019340. View the official record →
Linear boundary earthwork 370m east of Oscar Park Farm is a prehistoric or early historic linear earthwork located in Yorkshire, England. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1019340.
Linear boundary earthwork 370m east of Oscar Park 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 1019340.
Several scheduled monuments lie within 10 km, including Round barrow 710m NNE of Waterloo Farm, the southernmost of three round barrows in Far Moor Plantation (5.8 km), Round barrow on Scawton Moor, 700m ENE of High Lodge (5.9 km), Linear dyke known as Double Dikes, in Waterloo Plantation (6.1 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Linear boundary earthwork 370m east of Oscar Park 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.
Linear boundary earthwork 370m east of Oscar Park Farm stands on Corallian Group, bedrock that formed in the Oxfordian. The rock here is limestone, sandstone, siltstone and mudstone.