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Park pale known as Bishop's Dyke is a linear earthwork of medieval date located to the south and west of Furzy Brow in Hampshire. The dyke represents a park boundary, likely associated with land management and estate division during the medieval period. In the same locality, a Bronze Age bowl barrow survives as a burial mound, indicating prehistoric use of the landscape and settlement patterns from the second millennium before Christ. Together these monuments demonstrate the layered archaeological record of the Hampshire landscape, with Bronze Age funerary practices followed by medieval land organisation on the same terrain.
Park pale known as Bishop's Dyke, and a Bronze Age bowl barrow, to the south and west of Furzy Brow is a scheduled monument protected by Historic England under reference 1009324. View the official record →
Park pale known as Bishop's Dyke is a linear earthwork of medieval date located to the south and west of Furzy Brow in Hampshire. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1009324.
Park pale known as Bishop's Dyke, and a Bronze Age bowl barrow, to the south and west of Furzy Brow 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 1009324.
Several scheduled monuments lie within 10 km, including Bowl barrow and length of field boundary on Peaked Hill, 440m south-west of East Boldre Vicarage (6.2 km), Two bowl barrows 460m north-west of Norley Inclosure (6.2 km), Bowl barrow 400m north-west of Norley Inclosure (6.3 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Park pale known as Bishop's Dyke, and a Bronze Age bowl barrow, to the south and west of Furzy Brow'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.
Park pale known as Bishop's Dyke, and a Bronze Age bowl barrow, to the south and west of Furzy Brow stands on Bracklesham Group And Barton Group (Undifferentiated), bedrock that formed in the Eocene. The rock here is sand, silt and clay.