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Steyning Round Hill is a Bronze Age or Iron Age earthwork monument located near Steyning in West Sussex. The site comprises a series of barrows and associated ditches that represent funerary and possibly ceremonial activity during prehistory. The earthworks, though partially degraded, remain visible as low mounds and linear features in the landscape, evidence of the settlement and burial practices of early communities in the South Downs region. The monument's exact dating and functional interpretation continue to reflect the broader patterns of prehistoric land use documented across Sussex, though local archaeological investigation has provided insights into the character and preservation of this Bronze Age or Iron Age complex.
Barrows and ditches on Steyning Round Hill is a scheduled monument protected by Historic England under reference 1005852. View the official record →
Steyning Round Hill is a Bronze Age or Iron Age earthwork monument located near Steyning in West Sussex. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1005852.
Barrows and ditches on Steyning Round Hill 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 1005852.
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 (1.9 km), Cross dyke on Steep Down, 700m north east of Beggars Bush (2.7 km), Cross dyke on Steep Down, 600m north east of Titch Hill Farm (3.4 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Barrows and ditches on Steyning Round Hill'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.
Barrows and ditches on Steyning Round Hill stands on White Chalk Subgroup, bedrock that formed in the Maastrichtian. The rock here is chalk.