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Two of a dispersed group of five barrows adjacent to the Imber-Warminster track is a Bronze Age funerary monument located in Wiltshire. The barrows form part of a linear cemetery arrangement positioned along an ancient trackway connecting the settlements of Imber and Warminster. These earthworks represent typical Bronze Age burial practice, wherein round barrows served as communal or elite burial monuments constructed across the chalk downland landscape. The survival of five barrows in close association along this historically significant route demonstrates the importance of the Imber-Warminster track as a prehistoric routeway and ceremonial landscape.
Two of a dispersed group of five barrows adjacent to the Imber-Warminster track is a scheduled monument protected by Historic England under reference 1010056. View the official record →
Two of a dispersed group of five barrows adjacent to the Imber-Warminster track is a Bronze Age funerary monument located in Wiltshire. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1010056.
Two of a dispersed group of five barrows adjacent to the Imber-Warminster track 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 1010056.
Several scheduled monuments lie within 10 km, including Corton long barrow (8.4 km), Codford Circle hilltop enclosure (8.7 km), Strip lynchets immediately south west of Woodcombe Cleve (8.9 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Two of a dispersed group of five barrows adjacent to the Imber-Warminster track'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.
Two of a dispersed group of five barrows adjacent to the Imber-Warminster track stands on White Chalk Subgroup, bedrock that formed in the Maastrichtian. The rock here is chalk.