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Finchale Priory is a Benedictine cell established as a hermitage in the twelfth century on the River Wear near Durham. Founded by Saint Godric as a place of solitary religious retreat, it later developed into a monastic community under the jurisdiction of Durham Cathedral Priory. The substantial remains include the priory church, residential buildings, and evidence of the watermill that exploited the river's power to serve the establishment. The site represents an important example of a dependent monastic house, combining the spiritual tradition of anchoritic retreat with the practical economy of a working priory within the Durham ecclesiastical landscape.
Finchale Priory Benedictine cell: hermitage, monastic precinct and site of priory watermill is a scheduled monument protected by Historic England under reference 1007561. View the official record →
Finchale Priory is a Benedictine cell established as a hermitage in the twelfth century on the River Wear near Durham. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1007561.
Finchale Priory Benedictine cell: hermitage, monastic precinct and site of priory watermill 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 1007561.
Several scheduled monuments lie within 10 km, including Chapel of St Mary Magdalene (4.4 km), Elvet Bridge (5.1 km), Framwellgate Bridge (5.2 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Finchale Priory Benedictine cell: hermitage, monastic precinct and site of priory watermill'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.
Finchale Priory Benedictine cell: hermitage, monastic precinct and site of priory watermill stands on Pennine Middle Coal Measures Formation And South Wales Middle Coal Measures Formation (Undifferentiated), bedrock that formed in the Moscovian. The rock here is mudstone, siltstone, sandstone, coal, ironstone and ferricrete.