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White Sheet Downs Causewayed Camp is a Neolithic earthwork located in Somerset, England. The monument consists of multiple concentric circuits of banks and ditches with characteristic causeways or gaps interrupting the ditched lines, a defining feature of causewayed camps dating to the Early Neolithic period, approximately 3700–3400 BCE. Such camps are thought to have served communal purposes including seasonal gathering places, markets, or ceremonial centres rather than permanent settlements, and they represent some of the earliest monumental constructions in Britain. The site at White Sheet Downs survives as a substantial example of this monument type, preserving valuable evidence of Neolithic social organisation and land use in south-western England.
Neolithic causewayed camp, White Sheet Downs is a scheduled monument protected by Historic England under reference 1005640. View the official record →
White Sheet Downs Causewayed Camp is a Neolithic earthwork located in Somerset, England. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1005640.
Neolithic causewayed camp, White Sheet Downs 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 1005640.
Several scheduled monuments lie within 10 km, including Four bowl barrows on Long Hill, 220m west of Mere Castle (2.7 km), Mere Castle (2.7 km), Orchard Castle (4.6 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Neolithic causewayed camp, White Sheet Downs'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.
Neolithic causewayed camp, White Sheet Downs stands on White Chalk Subgroup, bedrock that formed in the Maastrichtian. The rock here is chalk.