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The hydro-electric power house and associated weir 250 metres north-west of Tin Bridge is a twentieth-century industrial structure constructed to harness water power for electricity generation. The installation reflects the early development of hydro-electric schemes in Yorkshire during a period of expanding industrial and domestic electrification. The weir and power house represent the technological infrastructure that characterised rural electrification projects undertaken in the early to mid-twentieth century. The site documents the transition from nineteenth-century water mill technology to modern electrical power generation on the watercourse.
Hydro-electric power house and associated weir 250m north west of Tin Bridge is a scheduled monument protected by Historic England under reference 1020895. View the official record →
The hydro-electric power house and associated weir 250 metres north-west of Tin Bridge is a twentieth-century industrial structure constructed to harness water power for electricity generation. It is designated a Scheduled Ancient Monument by Historic England (NHLE) under reference 1020895.
Hydro-electric power house and associated weir 250m north west of Tin Bridge 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 1020895.
Several scheduled monuments lie within 10 km, including Linton churchyard cross and sundial (0.6 km), Redmayne packhorse bridge (0.8 km), Medieval farmstead and field system, 530m south east of The Grange (1.2 km).
This page is just one thread. A full Aubrey report pulls together 15 strands of Hydro-electric power house and associated weir 250m north west of Tin Bridge'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.
Hydro-electric power house and associated weir 250m north west of Tin Bridge stands on Dinantian Rocks (Undifferentiated), bedrock that formed in the Mississippian. The rock here is limestone with subordinate sandstone and argillaceous rocks.