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The Romano-British field system 420 metres south-east of Roystone Grange is a scheduled ancient monument in Derbyshire comprising evidence of agricultural organisation dating to the Roman period. The site preserves traces of field boundaries and cultivation patterns characteristic of Romano-British rural settlement, reflecting the farming practices and land use of the Romano-British population in this region. The field system represents an important archaeological record of how the landscape was utilised and managed during the Roman occupation of Britain, complementing the understanding of settlement patterns in the wider Roystone Grange area.
Romano-British field system, 420m south east of Roystone Grange is a scheduled monument protected by Historic England under reference 1018089. View the official record →
The Romano-British field system 420 metres south-east of Roystone Grange is a scheduled ancient monument in Derbyshire comprising evidence of agricultural organisation dating to the Roman period.
Romano-British field system, 420m south east of Roystone Grange 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 1018089.
Several scheduled monuments lie within 10 km, including Medieval settlement, including fishpond and open field system, immediately north and 240m south of Lea Cottage Farm (4.6 km), Bank Top bowl barrow (4.9 km), Civil War redoubt 150m east of Tissington Hall (5 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Romano-British field system, 420m south east of Roystone Grange'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 field system, 420m south east of Roystone Grange stands on Dinantian Rocks (Undifferentiated), bedrock that formed in the Mississippian. The rock here is limestone with subordinate sandstone and argillaceous rocks.