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Antonine Wall at Seabegs Wood is a Roman frontier fortification constructed across central Scotland in the second century AD. The monument comprises a substantial rampart, parallel ditch and Military Way, forming part of the turf-built wall that stretched for approximately 37 miles between the Firth of Forth and Firth of Clyde. At this location in Stirlingshire, the defensive structures were constructed upon bedrock of the Clackmannan Group, Westphalian sedimentary formations that provided a stable foundation for the earthwork.
The rampart and ditch configuration at Seabegs Wood represents standard frontier engineering practice of the Roman period. The Military Way, running alongside the wall, facilitated troop movement and supply along the frontier line. The scale of the earthworks remains impressive despite nearly two millennia of weathering and agricultural use.
The site is protected as a scheduled monument by Historic Environment Scotland (reference SM90014), recognising its archaeological and historical significance as part of one of the most important Roman monuments in Britain. The remains at Seabegs Wood are among the best-preserved sections of the Antonine Wall and continue to provide insights into Roman military organisation and construction techniques in the northern frontier zone.
Antonine Wall, Seabegs Wood, rampart, ditch and Military Way is a scheduled monument protected by Historic Environment Scotland under reference SM90014. View the official record →
Antonine Wall at Seabegs Wood is a Roman frontier fortification constructed across central Scotland in the second century AD. It is designated a Scheduled Ancient Monument by Historic Environment Scotland under reference SM90014.
Antonine Wall, Seabegs Wood, rampart, ditch and Military Way is a Scheduled Ancient Monument, legally protected by Historic Environment Scotland — the body responsible for designating and safeguarding heritage sites in Scotland. The official designation reference is SM90014.
Several scheduled monuments lie within 10 km, including Antonine Wall, Dalnair to Seabegs Wood, including fortlet and camp (0.6 km), Antonine Wall, 80m SW of Woodhouse Eaves to Underwood Cottage (1.7 km), Castlecary House, souterrain 150m ESE of (2.5 km).
This page is just one thread. A full Aubrey report pulls together 14 strands of Antonine Wall, Seabegs Wood, rampart, ditch and Military Way'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.
Antonine Wall, Seabegs Wood, rampart, ditch and Military Way stands on Clackmannan Group, bedrock that formed in the Westphalian. The rock here is sedimentary rock cycles, clackmannan group type.