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A Romano-British farmstead and associated trackway is located 620 metres south-west of Bell Nook in Westmorland, England. The site consists of the remains of a Romano-British agricultural settlement typical of rural settlement patterns in the north of Roman Britain, dating to the Roman period. The farmstead is accompanied by an ancient trackway, indicating the presence of organised land use and communication routes serving the local settlement and its economic activities. The monument represents evidence of Romano-British rural occupation and land management in the upland regions of the north-west of England during the Roman conquest and subsequent administrative period.
Romano-British farmstead and associated trackway 620m south west of Bell Nook is a scheduled monument protected by Historic England under reference 1020343. View the official record →
A Romano-British farmstead and associated trackway is located 620 metres south-west of Bell Nook in Westmorland, England. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1020343.
Romano-British farmstead and associated trackway 620m south west of Bell Nook 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 1020343.
Several scheduled monuments lie within 10 km, including Great Musgrave shrunken medieval village (4.4 km), Water Houses clapper bridge (8.5 km), Rookby Scarth medieval settlement (8.9 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Romano-British farmstead and associated trackway 620m south west of Bell Nook'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 farmstead and associated trackway 620m south west of Bell Nook stands on Triassic Rocks (Undifferentiated), bedrock that formed in the Triassic. The rock here is sandstone and conglomerate, interbedded.