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Beech Bottom Dyke is a linear earthwork located in Hertfordshire, forming part of the Iron Age defensive and territorial infrastructure of the region. The monument consists of a substantial bank and ditch system that served to demarcate boundaries and control movement across the landscape during the Iron Age period. Such dykes functioned as both practical barriers and symbolic markers of territorial division, reflecting the organized settlement patterns and social structures of Iron Age communities in southern Britain. The earthwork remains visible as an archaeological feature, preserving evidence of prehistoric land management and inter-community organization.
Iron Age territorial boundary known as Beech Bottom Dyke is a scheduled monument protected by Historic England under reference 1019136. View the official record →
Beech Bottom Dyke is a linear earthwork located in Hertfordshire, forming part of the Iron Age defensive and territorial infrastructure of the region. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1019136.
Iron Age territorial boundary known as Beech Bottom Dyke 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 1019136.
Several scheduled monuments lie within 10 km, including The Clock Tower (2.7 km), St Albans Abbey Gatehouse (2.9 km), Verulamium, site of (3.1 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Iron Age territorial boundary known as Beech Bottom Dyke'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.
Iron Age territorial boundary known as Beech Bottom Dyke stands on White Chalk Subgroup, bedrock that formed in the Maastrichtian. The rock here is chalk.