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The enclosed settlement 290 metres south-east of Butteryhaugh Bridge is a Romano-British monument situated in Northumberland. The site comprises an enclosure of Romano-British date, representing a form of settlement typical of the rural economy of northern Britain during the Roman occupation period. Such enclosed settlements served domestic and agricultural functions for native British communities, often situated on the lower slopes or valleys where access to water and arable land was available. The monument survives as an archaeological earthwork and constitutes an important record of Romano-British settlement patterns in the region.
Romano-British enclosed settlement, 290m south east of Butteryhaugh Bridge is a scheduled monument protected by Historic England under reference 1009667. View the official record →
The enclosed settlement 290 metres south-east of Butteryhaugh Bridge is a Romano-British monument situated in Northumberland. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1009667.
Romano-British enclosed settlement, 290m south east of Butteryhaugh Bridge 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 1009667.
Several scheduled monuments lie within 10 km, including Kielder Viaduct (0.4 km), Two round cairns 870m south east of Butteryhaugh Bridge including Deadman Cairn (0.6 km), Devil's Lapful Long Cairn, 1km east of Butteryhaugh Bridge (0.7 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Romano-British enclosed settlement, 290m south east of Butteryhaugh Bridge'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.
Romano-British enclosed settlement, 290m south east of Butteryhaugh Bridge stands on Border Group, bedrock that formed in the Meramecian. The rock here is sandstone with subordinate argillaceous rocks and limestone.