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Hanging Grimston barrow group is a Bronze Age burial monument located approximately 200 metres west of Wold Farm in Yorkshire, England. The site comprises a bowl barrow, a common funerary monument type characteristic of the Bronze Age period, constructed as a simple earthen mound over an inhumed burial. The barrow group sits within the broader landscape of prehistoric burial sites that characterise the Yorkshire Wolds, a region rich in archaeological remains from the second and early third millennia before the Christian era. The monument remains a significant record of Bronze Age burial practice and territorial occupation patterns in northern England.
Hanging Grimston barrow group: a bowl barrow 200m west of Wold Farm is a scheduled monument protected by Historic England under reference 1007920. View the official record →
Hanging Grimston barrow group is a Bronze Age burial monument located approximately 200 metres west of Wold Farm in Yorkshire, England. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1007920.
Hanging Grimston barrow group: a bowl barrow 200m west 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 1007920.
Several scheduled monuments lie within 10 km, including Section of linear boundary dyke on Cow Moor, Millington Dale (8.4 km), Round barrow 400m north-west of Cobdale Farm (8.9 km), Round barrow 360m south-west of High Barn Farm (9.1 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Hanging Grimston barrow group: a bowl barrow 200m west 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.
Hanging Grimston barrow group: a bowl barrow 200m west of Wold Farm stands on White Chalk Subgroup, bedrock that formed in the Maastrichtian. The rock here is chalk.