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Heslerton Brow barrow group is a Bronze Age burial monument comprising three bowl barrows situated approximately 300 metres north-east of Wold Barn in Yorkshire, England. The three mounds represent typical examples of bowl barrow construction, the most common form of burial monument on the Yorkshire Wolds during the Bronze Age. These barrows formed part of the extensive cemetery landscapes that characterised the Wolds region during the second millennium BC, reflecting the funerary practices and social organisation of Bronze Age communities in this area.
Heslerton Brow barrow group: three bowl barrows 300m north-east of Wold Barn is a scheduled monument protected by Historic England under reference 1011586. View the official record →
Heslerton Brow barrow group is a Bronze Age burial monument comprising three bowl barrows situated approximately 300 metres north-east of Wold Barn in Yorkshire, England. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1011586.
Heslerton Brow barrow group: three bowl barrows 300m north-east of Wold Barn 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 1011586.
Several scheduled monuments lie within 10 km, including Thirkleby medieval settlement adjacent to Thirkleby Manor (6.4 km), Esh's round barrow: a long barrow and later bowl barrow 400m north of Cross Thorns Barn (7.1 km), Kirby Grindalythe medieval settlement earthworks immediately south west of St Andrew's Church (7.8 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Heslerton Brow barrow group: three bowl barrows 300m north-east of Wold Barn'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.
Heslerton Brow barrow group: three bowl barrows 300m north-east of Wold Barn stands on White Chalk Subgroup, bedrock that formed in the Maastrichtian. The rock here is chalk.