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Slight univallate hillfort on Swinhope Hill 430m north west of Glen Innes House is a prehistoric fortified settlement located in Lincolnshire. The monument comprises a single rampart enclosing an area of raised ground, characteristic of univallate hillfort construction in Iron Age Britain. The earthwork, though modest in surviving relief, represents a defensive settlement typical of the later prehistoric period in the East Midlands region. The site's location on elevated terrain reflects the strategic positioning favoured by Iron Age communities in establishing control over the surrounding landscape.
Slight univallate hillfort on Swinhope Hill 430m north west of Glen Innes House is a scheduled monument protected by Historic England under reference 1018839. View the official record →
Slight univallate hillfort on Swinhope Hill 430m north west of Glen Innes House is a prehistoric fortified settlement located in Lincolnshire. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1018839.
Slight univallate hillfort on Swinhope Hill 430m north west of Glen Innes House 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 1018839.
Several scheduled monuments lie within 10 km, including Remains of the Medieval Settlement of West Wykeham (6.2 km), Bowl barrow 100m south west of Gally Hill Farm (6.5 km), Remains of the Medieval Settlement of East Wykeham (6.6 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Slight univallate hillfort on Swinhope Hill 430m north west of Glen Innes House'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.
Slight univallate hillfort on Swinhope Hill 430m north west of Glen Innes House stands on Grey Chalk Subgroup, bedrock that formed in the Cenomanian. The rock here is chalk.