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Antonine Wall is a Roman frontier fortification built across central Scotland in the second century AD. This section, preserved between Buchley and Buchley Lodge in Lanarkshire, forms part of the turf-built rampart that originally extended 37 miles from the Firth of Forth to the Firth of Clyde. Constructed under the Roman Emperor Antoninus Pius, the wall incorporated a substantial ditch to its north and associated military infrastructure including forts and fortlets positioned at regular intervals along its length.
The monument sits on bedrock of the Clackmannan Group, sedimentary rocks formed during the Westphalian period. The underlying geology has influenced both the original construction method and the wall's survival, with the turf superstructure having largely degraded over nearly two millennia, leaving the ditch as the most visible topographical feature across much of the Lanarkshire landscape.
This section of the Antonine Wall is protected as a scheduled monument by Historic Environment Scotland under reference SM7547. The wall represents the northernmost frontier of the Roman Empire at its greatest extent and provides important evidence for Roman military engineering, logistics and settlement patterns in Scotland during the occupation of the 140s to 160s AD.
Antonine Wall, 270m S of Buchley to 25m SW of Buchley Lodge is a scheduled monument protected by Historic Environment Scotland under reference SM7547. View the official record →
Antonine Wall is a Roman frontier fortification built across central Scotland in the second century AD. It is designated a Scheduled Ancient Monument by Historic Environment Scotland under reference SM7547.
Antonine Wall, 270m S of Buchley to 25m SW of Buchley Lodge 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 SM7547.
Several scheduled monuments lie within 10 km, including Antonine Wall, 120m NE of Balmuildy Cottages to 270m S of Buchley (0.6 km), Forth and Clyde Canal: Bishopbriggs Golf Course (1 km), Antonine Wall, River Kelvin to 120m NE of Balmuildy Cottages (1.4 km).
This page is just one thread. A full Aubrey report pulls together 14 strands of Antonine Wall, 270m S of Buchley to 25m SW of Buchley Lodge'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, 270m S of Buchley to 25m SW of Buchley Lodge stands on Clackmannan Group, bedrock that formed in the Westphalian. The rock here is sedimentary rock cycles, clackmannan group type.