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The Forth and Clyde Canal, Bishopbriggs to Kirkintilloch, is a section of the major eighteenth-century navigation that connected the Firth of Forth to the Firth of Clyde across central Scotland. Completed in 1790, this canal section represents an important example of late Georgian civil engineering and served as a vital commercial waterway for transporting coal, iron, and other industrial goods throughout the nineteenth century. The canal is characterised by its stone-lined channel, accompanying towpath, and associated lock structures that facilitated the movement of vessels across the landscape. This stretch exemplifies the infrastructure that supported the industrial development of the central Belt during the eighteenth and nineteenth centuries and remains a significant archaeological monument of Scotland's transport heritage.
Forth and Clyde Canal: Bishopbriggs - Kirkintilloch is a scheduled monument protected by Historic Environment Scotland under reference SM6770. View the official record →
The Forth and Clyde Canal, Bishopbriggs to Kirkintilloch, is a section of the major eighteenth-century navigation that connected the Firth of Forth to the Firth of Clyde across central Scotland. It is designated a Scheduled Ancient Monument by Historic Environment Scotland under reference SM6770.
Forth and Clyde Canal: Bishopbriggs - Kirkintilloch 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 SM6770.
Several scheduled monuments lie within 10 km, including Antonine Wall, 270m S of Buchley to 25m SW of Buchley Lodge (2.9 km), Forth and Clyde Canal: Bishopbriggs Golf Course (3.2 km), Antonine Wall, 120m NE of Balmuildy Cottages to 270m S of Buchley (3.6 km).
This page is just one thread. A full Aubrey report pulls together 14 strands of Forth and Clyde Canal: Bishopbriggs - Kirkintilloch'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.
Forth and Clyde Canal: Bishopbriggs - Kirkintilloch stands on Clackmannan Group, bedrock that formed in the Westphalian. The rock here is sedimentary rock cycles, clackmannan group type.