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Moated site 140m east of St Mary's Church is a medieval defensive earthwork located in Shropshire. The monument consists of a substantial moat, a water-filled ditch that once enclosed a residential or manorial platform, representing a common form of high-status settlement protection during the medieval period. Such moated sites are typically dated to between the 12th and 16th centuries, reflecting the social hierarchy and fortification practices of medieval England. The survival of this earthwork provides archaeological evidence of medieval settlement patterns and domestic fortification in the region.
Moated site 140m east of St Mary's Church is a scheduled monument protected by Historic England under reference 1017238. View the official record →
Moated site 140m east of St Mary's Church is a medieval defensive earthwork located in Shropshire. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1017238.
Moated site 140m east of St Mary's Church 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 1017238.
Several scheduled monuments lie within 10 km, including Medieval fishpond reservoir NE of Haughmond Abbey and SW of the hamlet of Haughton (5 km), Haughmond Abbey: an Augustinian monastery on the site of an earlier religious foundation, a post-Dissolution residence and garden remains (6.2 km), Moated site, ridge and furrow cultivation remains and a building platform immediately north of Lower Grounds (6.2 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Moated site 140m east of St Mary's Church'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.
Moated site 140m east of St Mary's Church stands on Permian Rocks (Undifferentiated), bedrock that formed in the Permian. The rock here is sandstone and conglomerate, interbedded.