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Five Hill Field is a prehistoric barrow cemetery and cross dyke located 290 metres south west of Heath Farm in Cambridgeshire. The site comprises multiple burial mounds arranged within a defined field system marked by a cross dyke, a linear earthwork typical of Bronze Age land division. The barrows represent funerary monuments dating to the Bronze Age, reflecting organised cemetery practices and settlement patterns of the period. The survival of both the burial mounds and associated field boundary demonstrates the archaeological significance of this landscape in understanding prehistoric land use and social organisation in the East Anglian region.
Prehistoric barrow cemetery and cross dyke in Five Hill Field, 290m south west of Heath Farm is a scheduled monument protected by Historic England under reference 1020396. View the official record →
Five Hill Field is a prehistoric barrow cemetery and cross dyke located 290 metres south west of Heath Farm in Cambridgeshire. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1020396.
Prehistoric barrow cemetery and cross dyke in Five Hill Field, 290m south west of Heath Farm 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 1020396.
Several scheduled monuments lie within 10 km, including Moated site, Goodfellows. (5.8 km), Bush Wood moated site and hollow-way (5.8 km), Double moat and fishpond, Queenbury (5.9 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Prehistoric barrow cemetery and cross dyke in Five Hill Field, 290m south west of Heath Farm'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.
Prehistoric barrow cemetery and cross dyke in Five Hill Field, 290m south west of Heath Farm stands on White Chalk Subgroup, bedrock that formed in the Maastrichtian. The rock here is chalk.