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Gosbecks is a major Iron Age and Romano-British settlement site located near Colchester in Essex, England. The site comprises an extensive Iron Age oppidum with associated enclosures and field systems, later overlain by Romano-British occupation following the Roman conquest of Britain in AD 43. Archaeological investigation has revealed evidence of domestic settlement, craft activities, and ritual or ceremonial features spanning from the Late Iron Age through the Roman period, making it an important record of continuity and change during the transition from Iron Age society to Roman provincial life. The site's archaeology demonstrates the significance of the Colchester region as a major centre of settlement and economic activity in south-eastern Britain during this transformative period.
Gosbecks Iron Age and Romano-British site is a scheduled monument protected by Historic England under reference 1002180. View the official record →
Gosbecks is a major Iron Age and Romano-British settlement site located near Colchester in Essex, England. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1002180.
Gosbecks Iron Age and Romano-British site 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 1002180.
Several scheduled monuments lie within 10 km, including Dovecote 80m south west of Olivers (0.5 km), Remains of St Mary's Church (1.9 km), Berechurch Dyke: part of the Iron Age territorial oppidum and Romano-British town of Camulodunum (3.1 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Gosbecks Iron Age and Romano-British site'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.
Gosbecks Iron Age and Romano-British site stands on Thames Group, bedrock that formed in the Eocene. The rock here is clay, silt, sand and gravel.