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Barton Aqueduct is a masonry aqueduct carrying the Bridgewater Canal across the River Irwell in Lancashire, constructed between 1760 and 1761. Designed by James Brindley as part of the Duke of Bridgewater's pioneering canal scheme, the structure represents a major engineering achievement of the early canal age and exemplifies the innovative solutions required to navigate the challenging topography of the North West. The aqueduct comprises a substantial stone-built trunk spanning the river, supported on approach embankments and retaining walls that have been integral to its function for over two and a half centuries. As one of the earliest major aqueducts of the Industrial Revolution, Barton remains significant both as an engineering landmark and as a testament to the commercial ambitions that transformed the region's economy and infrastructure.
Bridgewater Canal's Barton Aqueduct embankment and retaining walls is a scheduled monument protected by Historic England under reference 1470478. View the official record →
Barton Aqueduct is a masonry aqueduct carrying the Bridgewater Canal across the River Irwell in Lancashire, constructed between 1760 and 1761. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1470478.
Bridgewater Canal's Barton Aqueduct embankment and retaining walls is a Scheduled Ancient Monument, legally protected by Historic England (NHLE) — the body responsible for designating and safeguarding heritage sites in England. The official designation reference is 1470478.
Several scheduled monuments lie within 10 km, including Lime kiln and associated culvert 50m north of Worsley Methodist Church (3 km), Canal tunnel entrances and wharf (3.4 km), Wardley Hall moated site, Worsley (4.6 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Bridgewater Canal's Barton Aqueduct embankment and retaining walls'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.
Bridgewater Canal's Barton Aqueduct embankment and retaining walls stands on Triassic Rocks (Undifferentiated), bedrock that formed in the Triassic. The rock here is sandstone and conglomerate, interbedded.