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Motte and bailey castle 90m west of St Mary Magdalene's Church, Quatford is a Norman fortification located in Shropshire. The monument comprises an earthwork motte with an adjoining bailey, typical of the castle typology established across England following the Norman Conquest of 1066. The site's proximity to Quatford Church and its topographical setting suggest strategic importance within the medieval settlement hierarchy of the Severn valley. The earthwork survives as a substantial landscape feature demonstrating the military and administrative authority exercised by Norman lords over the English countryside during the eleventh and twelfth centuries.
Motte and bailey castle 90m west of St Mary Magdalene's Church, Quatford is a scheduled monument protected by Historic England under reference 1019008. View the official record →
Motte and bailey castle 90m west of St Mary Magdalene's Church, Quatford is a Norman fortification located in Shropshire. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1019008.
Motte and bailey castle 90m west of St Mary Magdalene's Church, Quatford 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 1019008.
Several scheduled monuments lie within 10 km, including Panpudding Hill: a ringwork and bailey castle 100m south of Bridgnorth Station (2.8 km), The Hermitage (2.9 km), Bridgnorth Castle (2.9 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Motte and bailey castle 90m west of St Mary Magdalene's Church, Quatford'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.
Motte and bailey castle 90m west of St Mary Magdalene's Church, Quatford stands on Permian Rocks (Undifferentiated), bedrock that formed in the Permian. The rock here is sandstone and conglomerate, interbedded.