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The Queen Dike is a cross-dyke located approximately 600 metres east of Wold Farm in Yorkshire, England. The monument consists of an earthwork bank and ditch that traverses the landscape, forming part of a broader defensive or territorial boundary system typical of Iron Age settlement patterns in the region. The dike represents the kind of linear earthwork commonly constructed during the Iron Age period to demarcate land, control movement, or defend settled communities. As a scheduled ancient monument, the Queen Dike remains a significant archaeological feature for understanding Iron Age land use and settlement hierarchy in Yorkshire.
The Queen Dike: part of a cross-dyke 600m east of Wold Farm is a scheduled monument protected by Historic England under reference 1007919. View the official record →
The Queen Dike is a cross-dyke located approximately 600 metres east of Wold Farm in Yorkshire, England. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1007919.
The Queen Dike: part of a cross-dyke 600m east of 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 1007919.
Several scheduled monuments lie within 10 km, including Section of linear boundary dyke on Cow Moor, Millington Dale (8.3 km), Round barrow 390m south-west of High Barn Farm (8.7 km), Round barrow 400m north-west of Cobdale Farm (8.8 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of The Queen Dike: part of a cross-dyke 600m east of 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.
The Queen Dike: part of a cross-dyke 600m east of Wold Farm stands on White Chalk Subgroup, bedrock that formed in the Maastrichtian. The rock here is chalk.