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Three bowl barrows on Tulk's Hill is a Neolithic or Early Bronze Age funerary monument located approximately 800 metres north of East Bexington Farm in Dorset. The site comprises three distinct bowl-shaped burial mounds, a common form of funerary architecture across southern England during the third and second millennia before the present. Bowl barrows of this type typically contained inhumation burials, often accompanied by grave goods, and represent important evidence for settlement patterns and ritual practice in prehistoric Dorset. The monument's survival and scheduled protection reflect its significance as a Bronze Age landscape feature within the broader context of Dorset's archaeological heritage.
Three bowl barrows on Tulk's Hill 800m north of East Bexington Farm is a scheduled monument protected by Historic England under reference 1016374. View the official record →
Three bowl barrows on Tulk's Hill is a Neolithic or Early Bronze Age funerary monument located approximately 800 metres north of East Bexington Farm in Dorset. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1016374.
Three bowl barrows on Tulk's Hill 800m north of East Bexington Farm 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 1016374.
Several scheduled monuments lie within 10 km, including Two round barrows on Wears Hill (1.4 km), Four bowl barrows 725m ESE of Wears Farm (2.2 km), Dyke on Wears Hill (2.3 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Three bowl barrows on Tulk's Hill 800m north of East Bexington Farm'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.
Three bowl barrows on Tulk's Hill 800m north of East Bexington Farm stands on Gault Formation And Upper Greensand Formation (Undifferentiated), bedrock that formed in the Cenomanian. The rock here is mudstone, sandstone and limestone.