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Seven Barrows is a Bronze Age barrow cemetery located west of Clarendon Hill Reservoir in Hampshire, England. The site comprises multiple burial mounds characteristic of the Bronze Age period, representing an important concentration of funerary monuments from the second millennium before the present. Such barrow cemeteries are significant archaeological features that indicate sustained use of particular landscape locations for ritual and burial practices over extended periods. The monument is recorded on the National Heritage List for England under entry number 1015481, reflecting its recognised archaeological and historical importance within Hampshire's Bronze Age heritage.
Seven Barrows: a barrow cemetery west of Clarendon Hill Reservoir is a scheduled monument protected by Historic England under reference 1015481. View the official record →
Seven Barrows is a Bronze Age barrow cemetery located west of Clarendon Hill Reservoir in Hampshire, England. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1015481.
Seven Barrows: a barrow cemetery west of Clarendon Hill Reservoir 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 1015481.
Several scheduled monuments lie within 10 km, including Barrow cemetery 730m north of Hampshire Gap (8.3 km), Bowl barrow 780m NNE of Hampshire Gap (8.4 km), Bowl barrow within Boscombe Down Airfield, 160m south east of The Rifle and Pistol Club (9.2 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Seven Barrows: a barrow cemetery west of Clarendon Hill Reservoir'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.
Seven Barrows: a barrow cemetery west of Clarendon Hill Reservoir stands on White Chalk Subgroup, bedrock that formed in the Maastrichtian. The rock here is chalk.