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King's Quoit Burial Chamber is a Neolithic chambered tomb situated in Pembrokeshire, Wales, dating to the Neolithic period. The monument consists of a stone burial chamber with a distinctive dolmenic structure, comprising large upright stones supporting a substantial capstone, characteristic of passage graves and portal dolmens found throughout Wales and the broader Atlantic megalithic tradition. The site represents significant evidence of Neolithic funerary practice and communal burial customs in prehistoric Pembrokeshire, reflecting the ritual and religious beliefs of early farming communities in the region. As a Cadw-designated ancient monument, King's Quoit remains an important archaeological resource for understanding the megalithic heritage and monumental architecture of Neolithic Wales.
King's Quoit Burial Chamber is a scheduled monument protected by Cadw under reference PE035. View the official record →
King's Quoit Burial Chamber is a Neolithic chambered tomb situated in Pembrokeshire, Wales, dating to the Neolithic period. It is designated a Scheduled Ancient Monument by Cadw under reference PE035.
King's Quoit Burial Chamber dates from the prehistoric period, and is classified as a chambered tomb. It is one of over 32,000 scheduled monuments protected across the UK.
King's Quoit Burial Chamber 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 PE035.
Several scheduled monuments lie within 10 km, including Manorbier Dovecot (0.7 km), Manorbier Castle (0.7 km), Radar Station, Old Castle Head (1.6 km).
This page is just one thread. A full Aubrey report pulls together 13 strands of King's Quoit Burial Chamber'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.
King's Quoit Burial Chamber stands on Paleozoic sedimentary rocks, bedrock that formed in the Silurian. The rock here is sedimentary rocks.