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Halesowen Abbey is a Premonstratensian monastery founded in 1215 by the local lord Jocelin de Dinan in Worcestershire, establishing itself as one of the more significant religious houses in the West Midlands during the medieval period. The abbey maintained substantial landholdings and exercised considerable influence over local agriculture and water management throughout the thirteenth to sixteenth centuries. Physical remains include fragmentary stone foundations and earthwork features that indicate the layout of the monastic complex, whilst the surrounding landscape preserves evidence of the extensive water control systems, including fishponds and mill features, that the community engineered to support both subsistence and revenue generation. The site was dissolved under Henry VIII's Reformation programme in 1538, and the abbey lands subsequently passed into secular ownership, with the landscape features continuing to evolve through post-medieval agricultural use.
Halesowen Abbey and associated water control features is a scheduled monument protected by Historic England under reference 1009770. View the official record →
Halesowen Abbey is a Premonstratensian monastery founded in 1215 by the local lord Jocelin de Dinan in Worcestershire, establishing itself as one of the more significant religious houses in the West Midlands during the medieval period. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1009770.
Halesowen Abbey and associated water control 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 1009770.
Several scheduled monuments lie within 10 km, including Cross in St John the Baptist's churchyard (1.3 km), Moated site of Frankley Hall (3.1 km), Standing cross in St Leonards churchyard (3.3 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Halesowen Abbey and associated water control 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.
Halesowen Abbey and associated water control features stands on Warwickshire Group, bedrock that formed in the Early Permian. The rock here is mudstone, siltstone, sandstone, coal, ironstone and ferricrete.