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Part of Dorset Cursus is a Neolithic ceremonial earthwork located in Dorset, England, forming one of the longest cursuses in Britain. Constructed during the Early Neolithic period, approximately 3500 to 3000 BC, this monument consists of two parallel banks with external ditches extending across the landscape for several kilometres. The earthwork demonstrates the considerable communal labour and organisational capability of Neolithic communities, and likely served ceremonial or processional functions rather than defensive purposes. The surviving sections of the cursus remain visible as linear earthwork features in the Dorset landscape, constituting an important archaeological record of Neolithic monumental construction and territorial expression.
Part of Dorset Cursus is a scheduled monument protected by Historic England under reference 1003222. View the official record →
Part of Dorset Cursus is a Neolithic ceremonial earthwork located in Dorset, England, forming one of the longest cursuses in Britain. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1003222.
Part of Dorset Cursus 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 1003222.
Several scheduled monuments lie within 10 km, including Group of henge monuments, an associated group of round barrows, a Saxon cemetery, and a Norman church at Knowlton (6.4 km), Round barrow cemetery south of New Barn Farm, associated with the Knowlton Circles (6.8 km), Bowl barrow 170m north east of the Horton Inn (7.7 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Part of Dorset Cursus'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.
Part of Dorset Cursus stands on White Chalk Subgroup, bedrock that formed in the Maastrichtian. The rock here is chalk.