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Part of a Roman camp at Hoole, located 200 metres south of Hoole Hall in Cheshire, is a scheduled ancient monument comprising earthwork remains of a Roman military installation. The site preserves visible defensive ditches and other structural features characteristic of Roman temporary or semi-permanent camps of the Imperial period. Its precise dating and strategic function within the broader pattern of Roman occupation in north-west England remain subjects of archaeological study, though such installations typically relate to the campaigns and garrison activities of the first and second centuries AD. The monument's survival as earthworks makes it an important archaeological resource for understanding Roman military infrastructure in the region.
Part of a Roman camp at Hoole 200m south of Hoole Hall is a scheduled monument protected by Historic England under reference 1015129. View the official record →
Part of a Roman camp at Hoole, located 200 metres south of Hoole Hall in Cheshire, is a scheduled ancient monument comprising earthwork remains of a Roman military installation.
Part of a Roman camp at Hoole 200m south of Hoole Hall 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 1015129.
Several scheduled monuments lie within 10 km, including Huntington Hall moated site (4.5 km), Motte and associated earthworks east of Old Rectory (5.3 km), Moated site 180m W of Fir Tree Farm (5.7 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Part of a Roman camp at Hoole 200m south of Hoole Hall'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.
Part of a Roman camp at Hoole 200m south of Hoole Hall stands on Triassic Rocks (Undifferentiated), bedrock that formed in the Triassic. The rock here is sandstone and conglomerate, interbedded.