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Remains of Bixley Hall is a scheduled ancient monument comprising the substantial ruins of a substantial country house and its associated water features in Norfolk, England. The hall dates from the post-medieval period and represents a significant example of designed landscape gardening, with surviving evidence of formal water features including ponds and channels that once formed part of the estate's layout. The physical remains demonstrate the architectural and horticultural ambitions of its period, though the building itself now survives only as fragmentary ruins. The site retains archaeological value in its earthworks and subsurface deposits, which continue to inform understanding of post-medieval domestic settlement and landscape management in Norfolk.
Remains of Bixley Hall and associated garden water features is a scheduled monument protected by Historic England under reference 1018178. View the official record →
Remains of Bixley Hall is a scheduled ancient monument comprising the substantial ruins of a substantial country house and its associated water features in Norfolk, England.
Remains of Bixley Hall and associated garden water features 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 1018178.
Several scheduled monuments lie within 10 km, including Remains of medieval settlement 380m south of Park Farm (0.6 km), Remains of medieval settlement 400m east of Church Farm, Arminghall (0.7 km), Moated site at the Manor House, Arminghall (1.3 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Remains of Bixley Hall and associated garden water features'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.
Remains of Bixley Hall and associated garden water features stands on White Chalk Subgroup, bedrock that formed in the Maastrichtian. The rock here is chalk.