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Section of single linear boundary dyke in Stable Plantation, Greenwick Dale is a prehistoric or early medieval earthwork situated in the landscape of Yorkshire. The monument survives as a linear bank marking territorial or administrative boundaries in this part of northern England. Such dykes represent significant investments in landscape demarcation and would have served to define land ownership, control movement, or establish social boundaries during their period of use. The precise dating of this particular dyke remains uncertain without archaeological investigation, though similar linear earthworks in Yorkshire typically belong to either the Iron Age, Romano-British, or early Anglo-Saxon periods.
Section of single linear boundary dyke in Stable Plantation, Greenwick Dale, 400m south west of East Greenwick Farm is a scheduled monument protected by Historic England under reference 1015563. View the official record →
Section of single linear boundary dyke in Stable Plantation, Greenwick Dale is a prehistoric or early medieval earthwork situated in the landscape of Yorkshire. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1015563.
Section of single linear boundary dyke in Stable Plantation, Greenwick Dale, 400m south west of East Greenwick 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 1015563.
Several scheduled monuments lie within 10 km, including Round barrow 600m west of Newcote Farm (5.6 km), Site of Warter Augustinian Priory (6.2 km), Ousethorpe medieval settlement, moat and mill 310m south of Ousethorpe Farm (6.4 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Section of single linear boundary dyke in Stable Plantation, Greenwick Dale, 400m south west of East Greenwick 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 Stable Plantation, Greenwick Dale, 400m south west of East Greenwick Farm stands on White Chalk Subgroup, bedrock that formed in the Maastrichtian. The rock here is chalk.