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Cross Dyke on Mere Down is a linear earthwork situated east of White Sheet Hill hillfort in Wiltshire. The monument comprises a substantial bank and ditch alignment that dates to the Iron Age, representing a defensive or territorial boundary feature characteristic of that period. Such linear dykes served practical functions in regulating movement across the landscape and potentially demarcating land ownership or community boundaries during the later prehistoric period. The dyke's proximity to the nearby hillfort suggests it may have formed part of a wider system of fortified and controlled landscape features associated with Iron Age settlement hierarchies in this area of Wiltshire.
Cross dyke on Mere Down, east of White Sheet Hill hillfort is a scheduled monument protected by Historic England under reference 1017710. View the official record →
Cross Dyke on Mere Down is a linear earthwork situated east of White Sheet Hill hillfort in Wiltshire. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1017710.
Cross dyke on Mere Down, east of White Sheet Hill hillfort 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 1017710.
Several scheduled monuments lie within 10 km, including Mere Castle (2 km), Four bowl barrows on Long Hill, 220m west of Mere Castle (2.1 km), Orchard Castle (4.9 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Cross dyke on Mere Down, east of White Sheet Hill hillfort'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.
Cross dyke on Mere Down, east of White Sheet Hill hillfort stands on White Chalk Subgroup, bedrock that formed in the Maastrichtian. The rock here is chalk.