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Ring ditch 200 yards south-west of Trelease Mill is a prehistoric circular earthwork located in Cornwall. The monument comprises a roughly circular ditch with an associated bank, characteristic of ring ditches dating to the Bronze Age, a period when such enclosed ceremonial or domestic structures were commonly constructed across the British landscape. The precise function of this particular example remains uncertain, though ring ditches of this type are frequently interpreted as the denuded remains of barrows, domestic compounds, or ritual enclosures. The site's survival as an earthwork demonstrates the value of such monuments for understanding Bronze Age settlement patterns and land use in south-west England.
Ring ditch 200yds (180m) SW of Trelease Mill is a scheduled monument protected by Historic England under reference 1004333. View the official record →
Ring ditch 200 yards south-west of Trelease Mill is a prehistoric circular earthwork located in Cornwall. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1004333.
Ring ditch 200yds (180m) SW of Trelease Mill 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 1004333.
Several scheduled monuments lie within 10 km, including Hut circle with associated field system 100yds (90m) NNW of Poldowrian Farm (4.5 km), Promontory fort at Lankidden (5 km), Medieval chapel enclosure 340m south east of Hendra Farm (6.4 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Ring ditch 200yds (180m) SW of Trelease Mill'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.
Ring ditch 200yds (180m) SW of Trelease Mill stands on Devonian Rocks (Undifferentiated), bedrock that formed in the Devonian. The rock here is hornblende schist.