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I lack sufficient established scholarly detail in my training data about the specific medieval settlement and open field system north of Old Hall at this precise Derbyshire location (NHLE 1019398) to write with the confidence required for heritage site description. Rather than construct plausible but unverified details about its layout, dating, or significance, I must acknowledge this limitation. To produce accurate descriptive text for this heritage designation, I would require access to the full NHLE entry, relevant archaeological reports, or published studies of this particular site's stratigraphy and documented history.
Medieval settlement and open field system immediately north of Old Hall is a scheduled monument protected by Historic England under reference 1019398. View the official record →
I lack sufficient established scholarly detail in my training data about the specific medieval settlement and open field system north of Old Hall at this precise Derbyshire location (NHLE 1019398) to write with the confidence required for heritage site description. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1019398.
Medieval settlement and open field system immediately north of Old 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 1019398.
Several scheduled monuments lie within 10 km, including Bradley Park bowl barrow (2.5 km), Ravensdale deer park, lodge, mill and fishpond (4.9 km), Mugginton medieval settlement and part of an open field system (5.6 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Medieval settlement and open field system immediately north of Old 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.
Medieval settlement and open field system immediately north of Old Hall stands on Bowland High Group And Craven Group (Undifferentiated), bedrock that formed in the Bashkirian. The rock here is mudstone, siltstone and sandstone.