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The prehistoric linear boundary at Crown Tegleaze is a scheduled ancient monument comprising a substantial earthwork located approximately one kilometre north-west of Littleton Farm in Sussex. The monument consists of a linear ditch and bank formation characteristic of prehistoric boundary systems, likely dating to the Bronze Age or Iron Age periods when such linear features were commonly employed to demarcate territorial divisions, control livestock movement, or establish land ownership. The earthwork survives as a visible landscape feature and represents an important example of prehistoric land organisation in the Sussex region. The site's scheduled status reflects its archaeological significance as evidence of prehistoric settlement patterns and social organisation in southern Britain.
Prehistoric linear boundary at Crown Tegleaze, 1km north west of Littleton Farm is a scheduled monument protected by Historic England under reference 1015961. View the official record →
The prehistoric linear boundary at Crown Tegleaze is a scheduled ancient monument comprising a substantial earthwork located approximately one kilometre north-west of Littleton Farm in Sussex.
Prehistoric linear boundary at Crown Tegleaze, 1km north west of Littleton 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 1015961.
Several scheduled monuments lie within 10 km, including Long Down prehistoric flint mine (6 km), Causewayed enclosure, World War II searchlight emplacements and associated remains on Halnaker Hill (6.1 km), Halnaker House: a fortified medieval manor house and part of its landscaped grounds (7.1 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Prehistoric linear boundary at Crown Tegleaze, 1km north west of Littleton 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.
Prehistoric linear boundary at Crown Tegleaze, 1km north west of Littleton Farm stands on White Chalk Subgroup, bedrock that formed in the Maastrichtian. The rock here is chalk.