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St Constantine's cells is a site of rock-cut chambers located at Wetheral in Cumberland, situated within a sandstone cliff above the River Eden. The caves comprise a series of small cells carved into the natural rock face, traditionally associated with early Christian hermitic occupation, though their precise date of origin and original purpose remain matters of scholarly debate. A Roman inscription is present at the site, though its relationship to the cell system and its exact provenance within the archaeological context require careful interpretation. The monument represents evidence of both Romano-British activity and potential early medieval Christian use of the Wetheral locality.
St Constantine's cells (Wetheral Caves) and rock-cut Roman inscription is a scheduled monument protected by Historic England under reference 1007160. View the official record →
St Constantine's cells is a site of rock-cut chambers located at Wetheral in Cumberland, situated within a sandstone cliff above the River Eden. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1007160.
St Constantine's cells (Wetheral Caves) and rock-cut Roman inscription 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 1007160.
Several scheduled monuments lie within 10 km, including Wetheral Priory gatehouse and length of medieval wall (0.7 km), Scalesceugh Roman kilns (4.4 km), Park House Roman fort (4.6 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of St Constantine's cells (Wetheral Caves) and rock-cut Roman inscription'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.
St Constantine's cells (Wetheral Caves) and rock-cut Roman inscription stands on Triassic Rocks (Undifferentiated), bedrock that formed in the Triassic. The rock here is sandstone and conglomerate, interbedded.