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Llangattock Tramroad Inclines is a post-medieval industrial monument in Wales, protected by Cadw under reference BR234. The tramroad was engineered to transport stone and other materials across steep terrain, making use of gravity-assisted inclines characteristic of tramroad systems developed during the industrial expansion of South Wales. The structure exploited the dramatic topography of the Llangattock landscape, where the underlying Lower Devonian bedrock of interbedded sandstone and conglomerate creates marked natural slopes.
The inclines represent a significant phase of industrial transport development, predating the era of steam locomotives and designed for horse-drawn or gravity-powered operation. Such systems were crucial to the Welsh slate, coal and limestone industries, connecting quarries and mines with navigable waterways or rail networks below. The solid Devonian foundation beneath the site provided a stable base for the construction of these substantial earthworks.
Today the Llangattock Tramroad Inclines remain visible as engineered features within the Welsh landscape, evidence of the mechanical ingenuity applied to resource extraction and transport during the post-medieval industrial period. The monument's preservation reflects the importance of understanding how communities adapted the natural geology and topography to support industrial enterprise.
Llangattock Tramroad Inclines is a scheduled monument protected by Cadw under reference BR234. View the official record →
Llangattock Tramroad Inclines is a post-medieval industrial monument in Wales, protected by Cadw under reference BR234.
Llangattock Tramroad Inclines dates from the post medieval/modern period, and is classified as a tramroad. It is one of over 32,000 scheduled monuments protected across the UK.
Llangattock Tramroad Inclines is a Scheduled Ancient Monument, legally protected by Cadw — the body responsible for designating and safeguarding heritage sites in Wales. The official designation reference is BR234.
Several scheduled monuments lie within 10 km, including Brake Engine on Hill Pits Tramroad Incline (7.6 km), Pwll Du Tunnel (7.8 km), Old Coal Pits, Blaenavon (7.9 km).
This page is just one thread. A full Aubrey report pulls together 13 strands of Llangattock Tramroad Inclines'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.
Llangattock Tramroad Inclines stands on Lower Devonian Rocks (Undifferentiated), bedrock that formed in the Early Devonian. The rock here is sandstone and conglomerate, interbedded.