Embanked Aqueduct SW of Govilon ( including Wall & Gate-piers to W ) is a Grade II listed building in the Brecon Beacons National Park local planning authority area, Wales. First listed on 15 March 1996. Aqueduct.
Embanked Aqueduct SW of Govilon ( including Wall & Gate-piers to W )
- WRENN ID
- gilded-keep-summer
- Grade
- II
- Local Planning Authority
- Brecon Beacons National Park
- Constituency
- Monmouthshire MP: Catherine Fookes (Lab)
- Country
- Wales
- Date first listed
- 15 March 1996
- Type
- Aqueduct
- Address
- Embanked Aqueduct SW of Govilon ( including Wall & Gate-piers to W ), Llanfoist Fawr, Monmouthshire
- OS grid reference
- SO 263 136
- Coordinates
- 51.81693, -3.06942
- Source
- Cadw listing
Description
This is an embanked aqueduct, dating from 1805, and forming part of the Brecknock and Abergavenny Canal. The canal was promoted in 1792 to connect the upper Usk valley with the Monmouthshire Canal, and construction began in 1797, though completion of the section near Govilon was delayed until 1805, overseen by engineer Thomas Cartwright. Later, between 1809 and 1812, the canal was extended to Pontymoile. The canal was important for the transport of iron, lime, and coal, and was eventually absorbed into the Great Western Railway before being abandoned in 1962. Restoration work began in 1964 and continues.
The aqueduct follows the contours of the landscape, so embanked structures were used instead of locks to navigate sharp bends. This structure carries the canal around a corner, over a stream which flows beneath a segmental arch constructed with voussoirs. The downhill side features a high revetment of roughly coursed masonry. A flat parapet runs along the top, with pilaster strips at the ends. To the west, the parapets continue as a rubble wall, which borders the towpath around the bend and includes a pair of tall stone gate piers of unexplained purpose.
The aqueduct is listed as a scarce and well-preserved example of canal engineering on an important section of the canal.
Local climate
Embanked Aqueduct SW of Govilon ( including Wall & Gate-piers to W ) sits in a wetter-than-average part of the UK, with an average of 1,040 mm of rain a year. This makes it wetter than 83% of listed buildings in the UK. Its exposure to wind-driven rain is greater than that of 75% of listed buildings.
It experiences an average of 48 freeze-thaw cycles a year, more than 89% of listed buildings. Of these, 24 follow at least 1 mm of rain in the preceding 48 hours. Average temperatures at this location have risen by 0.3°C per decade since 1991.
Averages for 1991–2020; temperature trend 1991–2025. Figures describe the wider area (a grid cell of roughly 10 km), not the individual site. Contains modified Copernicus Climate Change Service information 2026.
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