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Buckden Gavel lead smelt mill and mine is a scheduled ancient monument located in Wharfedale, North Yorkshire, representing the industrial archaeology of lead extraction and processing in the Pennines. The site dates from the early modern period, with evidence of activity spanning the sixteenth to nineteenth centuries as part of the wider lead mining industry that exploited the mineral-rich geology of the Yorkshire Dales. The remains comprise both underground mine workings and the physical infrastructure associated with smelting operations, reflecting the technological approaches employed in ore processing during this era. This monument contributes significantly to understanding the history of non-ferrous metal extraction in northern England and the economic development of the upland regions during the early industrial period.
Buckden Gavel lead smelt mill and mine is a scheduled monument protected by Historic England under reference 1015905. View the official record →
Buckden Gavel lead smelt mill and mine is a scheduled ancient monument located in Wharfedale, North Yorkshire, representing the industrial archaeology of lead extraction and processing in the Pennines.
Buckden Gavel lead smelt mill and mine 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 1015905.
Several scheduled monuments lie within 10 km, including Shorn medieval boundary cross and bowl barrow (3.2 km), Tor Dike linear earthwork (3.6 km), Bowl barrow 120m north of Tor Dike on Little Hunters Sleets (3.9 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Buckden Gavel lead smelt mill and mine'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.
Buckden Gavel lead smelt mill and mine stands on Yoredale Group, bedrock that formed in the Bashkirian. The rock here is limestone with subordinate sandstone and argillaceous rocks.