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Remains of St Andrew's Chapel, located north west of Chapel Cross in Somerset, is a medieval religious structure whose fragmentary archaeological remains survive from the medieval period. The site preserves evidence of a small chapel, with physical traces indicating its former presence in the landscape despite substantial loss and degradation over the centuries. As a designated ancient monument, the remains represent an important record of rural religious provision and the extent of medieval ecclesiastical infrastructure in Somerset, contributing to understanding of local settlement patterns and spiritual life in the medieval countryside.
Remains of St Andrew's Chapel, 80m north west of Chapel Cross is a scheduled monument protected by Historic England under reference 1021120. View the official record →
Remains of St Andrew's Chapel, located north west of Chapel Cross in Somerset, is a medieval religious structure whose fragmentary archaeological remains survive from the medieval period. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1021120.
Remains of St Andrew's Chapel, 80m north west of Chapel Cross 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 1021120.
Several scheduled monuments lie within 10 km, including Dunkery Beacon and adjacent mounds (3.6 km), Cairn 850m north east of Dunkery Bridge (3.7 km), Round barrow 800yds (730m) SW of Dunkery Beacon (4.2 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Remains of St Andrew's Chapel, 80m north west of Chapel Cross'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.
Remains of St Andrew's Chapel, 80m north west of Chapel Cross stands on Triassic Rocks (Undifferentiated), bedrock that formed in the Triassic. The rock here is sandstone and conglomerate, interbedded.