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The pair of hlaews located 150 metres south-east of Chanctonbury Ring hillfort is a Bronze Age funerary monument situated on the South Downs in West Sussex. These burial mounds form part of the broader ceremonial landscape associated with Chanctonbury Ring, an Iron Age hillfort that was constructed at a later period than these Bronze Age features. The hlaews represent evidence of prehistoric burial practice and demonstrate the long-term ceremonial significance of this location on the South Downs, with successive periods of activity spanning from the Bronze Age through to the Iron Age.
Pair of hlaews 150m south east of Chanctonbury Ring hillfort is a scheduled monument protected by Historic England under reference 1015118. View the official record →
The pair of hlaews located 150 metres south-east of Chanctonbury Ring hillfort is a Bronze Age funerary monument situated on the South Downs in West Sussex. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1015118.
Pair of hlaews 150m south east of Chanctonbury Ring hillfort 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 1015118.
Several scheduled monuments lie within 10 km, including Regular aggregate field system with prehistoric and Romano-British farmsteads and a Bronze Age bowl barrow on Park Brow (3.3 km), Cissbury Ring hillfort, prehistoric flint mine and associated remains (3.9 km), Bowl barrow 120m north west of Cissbury (4.1 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Pair of hlaews 150m south east of Chanctonbury Ring hillfort'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.
Pair of hlaews 150m south east of Chanctonbury Ring hillfort stands on White Chalk Subgroup, bedrock that formed in the Maastrichtian. The rock here is chalk.