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Stott Park bobbin mill is a 19th-century industrial site located in Lancashire, England, which represents the specialised manufacture of wooden bobbins for the textile industry. The mill complex includes two mill ponds that provided the waterpower necessary to operate the machinery, alongside evidence of an earlier smithy that would have serviced the industrial operation. The bobbin mill itself dates from the industrial expansion of the 19th century, reflecting Lancashire's significance as a centre of textile-related manufacturing. The site demonstrates the integration of water-powered machinery, reservoir infrastructure, and ancillary metalworking facilities typical of rural Lancashire's industrial heritage.
Stott Park bobbin mill, two mill ponds and site of Stott Park smithy is a scheduled monument protected by Historic England under reference 1014936. View the official record →
Stott Park bobbin mill is a 19th-century industrial site located in Lancashire, England, which represents the specialised manufacture of wooden bobbins for the textile industry. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1014936.
Stott Park bobbin mill, two mill ponds and site of Stott Park smithy 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 1014936.
Several scheduled monuments lie within 10 km, including Newby Bridge (1.8 km), Backbarrow ironworks (3.8 km), Stony Hazel finery forge (3.9 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Stott Park bobbin mill, two mill ponds and site of Stott Park smithy'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.
Stott Park bobbin mill, two mill ponds and site of Stott Park smithy stands on Silurian Rocks (Undifferentiated), bedrock that formed in the Silurian. The rock here is mudstone, siltstone and sandstone.