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Antonine Wall, Millhall Burn to River Avon is a section of the most northerly frontier of the Roman Empire, constructed in the 140s AD under the Emperor Antoninus Pius. This stretch of turf-built rampart extends across Stirlingshire between the Millhall Burn and the River Avon, traversing bedrock of the Clackmannan Group, a formation of sedimentary rocks laid down during the Westphalian period of the Carboniferous era. The wall's base lies directly upon these ancient strata, which shaped both the construction methods available to Roman engineers and the landscape through which the fortification ran.
The Antonine Wall stretched approximately 37 miles across the Forth-Clyde isthmus, serving as a garrisoned military barrier for roughly two decades before being abandoned. This particular section demonstrates the wall's characteristic construction: a turf superstructure built upon stone foundations, accompanied by a substantial ditch to the north. The River Avon and Millhall Burn marked significant natural features in the Roman military landscape, providing water access and defensive advantages.
The site is protected by Historic Environment Scotland as Scheduled Monument SM9728, recognising its archaeological significance as part of one of Scotland's most important Roman remains. The survival of this section preserves evidence of Roman military engineering adapted to Scottish terrain and geology.
Antonine Wall, Millhall Burn to River Avon is a scheduled monument protected by Historic Environment Scotland under reference SM9728. View the official record →
Antonine Wall, Millhall Burn to River Avon is a section of the most northerly frontier of the Roman Empire, constructed in the 140s AD under the Emperor Antoninus Pius. It is designated a Scheduled Ancient Monument by Historic Environment Scotland under reference SM9728.
Antonine Wall, Millhall Burn to River Avon 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 SM9728.
Several scheduled monuments lie within 10 km, including Refuge Stone, 300m WNW of Westfield Farm, Westfield (7.2 km), Torphichen Preceptory, refuge stone at Torphichen Kirk (7.4 km), Torphichen Preceptory (7.4 km).
This page is just one thread. A full Aubrey report pulls together 14 strands of Antonine Wall, Millhall Burn to River Avon'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, Millhall Burn to River Avon stands on Clackmannan Group, bedrock that formed in the Westphalian. The rock here is sedimentary rock cycles, clackmannan group type.