© Mapbox · © OpenStreetMap contributors · Boundary data © Historic England (NHLE)
Roman piers and revetment in the River Itchen is a submerged archaeological monument located in Hampshire, comprising structural remains associated with Roman activity along the river. The features consist of timber and masonry elements that formed part of riverside infrastructure, likely serving port or landing facilities during the Roman occupation of Britain. The monument dates to the Roman period, reflecting the strategic importance of the Itchen as a navigable waterway for transport and commerce in the region. These remains represent significant evidence of Roman engineering and economic activity in southern Hampshire during antiquity.
Roman piers and revetment in the River Itchen is a scheduled monument protected by Historic England under reference 1425731. View the official record →
Roman piers and revetment in the River Itchen is a submerged archaeological monument located in Hampshire, comprising structural remains associated with Roman activity along the river. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1425731.
Roman piers and revetment in the River Itchen 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 1425731.
Several scheduled monuments lie within 10 km, including Bowl barrow 260m north of Stonyford Pond (9.5 km), Bowl barrow 220m north-east of Stonyford Pond (9.6 km), Bowl barrow 340m east of Harford House (9.6 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Roman piers and revetment in the River Itchen'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.
Roman piers and revetment in the River Itchen stands on Eocene claystone, bedrock that formed in the Eocene. The rock here is claystone.