© Mapbox · © OpenStreetMap contributors · Boundary data © Historic Environment Scotland
Mollins Roman fort is a Roman auxiliary fort located in Lanarkshire, Scotland, dating to the period of Roman occupation in Britain. The fort forms part of the defensive infrastructure associated with the Antonine Wall, the northernmost frontier of the Roman Empire constructed in the second century AD under the emperor Antoninus Pius. Archaeological investigation has identified the characteristic playing-card shaped plan typical of Roman forts, with evidence of ditches and ramparts that would have protected the garrison. The site represents an important example of Roman military architecture in Scotland and contributes to understanding the extent and organisation of Roman control during the Antonine period.
Mollins Roman fort is a scheduled monument protected by Historic Environment Scotland under reference SM6136. View the official record →
Mollins Roman fort is a Roman auxiliary fort located in Lanarkshire, Scotland, dating to the period of Roman occupation in Britain. It is designated a Scheduled Ancient Monument by Historic Environment Scotland under reference SM6136.
Mollins Roman fort 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 SM6136.
Several scheduled monuments lie within 10 km, including Forth and Clyde Canal: Kirkintilloch - Auchinstarry Farm (4.2 km), Drumbowie Farm, anti-aircraft battery, 350m WSW of (4.7 km), Antonine Wall and fort, 130m NE to 375m WSW of Auchendavie Farm (4.7 km).
This page is just one thread. A full Aubrey report pulls together 14 strands of Mollins Roman fort'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.
Mollins Roman fort stands on Clackmannan Group, bedrock that formed in the Westphalian. The rock here is sedimentary rock cycles, clackmannan group type.