Old Frackford Bridge is a Grade II listed building in the Exmoor National Park local planning authority area, England. First listed on 4 August 1983. Bridge.

Old Frackford Bridge

WRENN ID
eternal-eave-dale
Grade
II
Local Planning Authority
Exmoor National Park
Constituency
Tiverton and Minehead MP: Rachel Gilmour (LD)
Country
England
Date first listed
4 August 1983
Type
Bridge
Address
Old Frackford Bridge, Dunster, Somerset
OS grid reference
SS 984 432
Coordinates
51.17945, -3.454
Source
Historic England listing

Also on this page: flood risk · radon risk · weather exposure · detailed attributes ↓

Description

Old Frackford Bridge, dated 1768, was built by William and George Rawle. It is constructed of random rubble sandstone and features two semi-circular arches. The bridge has later triangular coping on its parapets, which were partly overgrown with ivy at the time of the survey. The date and builders' names are carved on a slate let into the east face of the bridge. It is no longer in use, having been replaced by a single span bridge in 1913.

Local climate

Old Frackford Bridge sits in a wetter-than-average part of the UK, with an average of 1,130 mm of rain a year. This makes it wetter than 88% of listed buildings in the UK. Its exposure to wind-driven rain is greater than that of 95% of listed buildings.

It experiences an average of 10 freeze-thaw cycles a year, fewer than 90% of listed buildings. Of these, 5 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.

More on this building

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  • Detailed attributes — period, style, materials, features
  • Flood risk assessment
  • Radon risk assessment
  • Weather exposure and heating demand — rain and frost month by month and year by year, wind direction, solar and humidity
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