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The Forth and Clyde Canal Glasgow Branch is a navigable waterway constructed in the late eighteenth century as an extension of the principal Forth and Clyde Canal, linking Glasgow to the main canal system. The branch was engineered to provide direct access from Glasgow to the central belt canal network, facilitating the transport of coal, minerals, and manufactured goods between the city and eastern Scotland. The waterway remains substantially intact as a physical monument to eighteenth-century civil engineering and represents an important component of Scotland's industrial heritage infrastructure. The canal's survival as a navigable waterway and its role in Glasgow's commercial development during the Industrial Revolution underscore its historical and archaeological significance.
Forth and Clyde Canal: Glasgow Branch is a scheduled monument protected by Historic Environment Scotland under reference SM6771. View the official record →
The Forth and Clyde Canal Glasgow Branch is a navigable waterway constructed in the late eighteenth century as an extension of the principal Forth and Clyde Canal, linking Glasgow to the main canal system. It is designated a Scheduled Ancient Monument by Historic Environment Scotland under reference SM6771.
Forth and Clyde Canal: Glasgow Branch 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 SM6771.
Several scheduled monuments lie within 10 km, including North Woodside Flint Mills,Garriochmill Road,North Kelvin (0.8 km), Forth and Clyde Canal: Cleveden Road - Bishopbriggs Golf Course (1.5 km), Forth and Clyde Canal, Port Dundas canal basin, Glasgow (1.9 km).
This page is just one thread. A full Aubrey report pulls together 14 strands of Forth and Clyde Canal: Glasgow Branch'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: Glasgow Branch stands on Clackmannan Group, bedrock that formed in the Westphalian. The rock here is sedimentary rock cycles, clackmannan group type.