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The Roman camp 200 metres west of Galleygill Bridge is a temporary marching camp of the Roman period, situated in Cumberland in northern England. The site represents one of the auxiliary camps associated with Roman military operations in the region, likely dating to the period of intensive campaigning during the first and second centuries AD. The camp's earthworks, though subject to erosion and agricultural use over nearly two millennia, retain sufficient topographical definition to indicate its characteristic playing-card layout and defensive ditches typical of Roman military installations. Its location within the broader context of Roman frontier infrastructure reflects the strategic importance of northern England during the Roman occupation of Britain.
Roman camp 200m west of Galleygill Bridge is a scheduled monument protected by Historic England under reference 1007869. View the official record →
The Roman camp 200 metres west of Galleygill Bridge is a temporary marching camp of the Roman period, situated in Cumberland in northern England. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1007869.
Roman camp 200m west of Galleygill 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 1007869.
Several scheduled monuments lie within 10 km, including Bowl barrow 350m north east of The Wreay (8.4 km), Long cairn 370m ESE of Mossthorn Farm (8.5 km), Sewborrans standing stone 400m south west of Sewborwens (8.9 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Roman camp 200m west of Galleygill 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.
Roman camp 200m west of Galleygill Bridge stands on Permian Rocks (Undifferentiated), bedrock that formed in the Permian. The rock here is sandstone and conglomerate, interbedded.