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Tintern Abbey is a Cistercian monastery founded in 1131 in the Wye Valley, Monmouthshire, Wales, by Norman knights of the FitzGerald family. The standing remains date predominantly from the thirteenth and fourteenth centuries, representing successive phases of architectural expansion typical of wealthy Cistercian houses, including a notably intact west front and soaring Gothic windows. The abbey functioned as a major religious and economic centre throughout the medieval period until its dissolution in 1536 during Henry VIII's Reformation. The picturesque ruins, which inspired considerable Romantic artistic interest from the eighteenth century onwards, survive as one of Wales's most substantial monastic remains and preserve important evidence of medieval monastic architecture and liturgical arrangement.
Tintern Abbey is a scheduled monument protected by Cadw under reference MM102. View the official record →
Tintern Abbey is a Cistercian monastery founded in 1131 in the Wye Valley, Monmouthshire, Wales, by Norman knights of the FitzGerald family. It is designated a Scheduled Ancient Monument by Cadw under reference MM102.
Tintern Abbey dates from the medieval period, and is classified as a abbey. It is one of over 32,000 scheduled monuments protected across the UK.
Tintern Abbey is a Scheduled Ancient Monument, legally protected by Cadw — the body responsible for designating and safeguarding heritage sites in Wales. The official designation reference is MM102.
Several scheduled monuments lie within 10 km, including St Peter's Cave (7.4 km), Long Barrow and Round Barrow at Thornwell Farm (8.4 km), Runston Medieval Village Site & Runston Chapel (9.3 km).
This page is just one thread. A full Aubrey report pulls together 13 strands of Tintern Abbey'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.
Tintern Abbey stands on Upper Devonian Rocks (Undifferentiated), bedrock that formed in the Late Devonian. The rock here is sandstone and conglomerate, interbedded.