Corby Bridge is a Grade I listed building in the Cumberland local planning authority area, England. First listed on 1 April 1957. Bridge.
Corby Bridge
- WRENN ID
- white-brass-crow
- Grade
- I
- Local Planning Authority
- Cumberland
- Constituency
- Carlisle MP: Ms Julie Minns (Lab)
- Country
- England
- Date first listed
- 1 April 1957
- Type
- Bridge
- Address
- Corby Bridge, Wetheral
- OS grid reference
- NY 468 546
- Coordinates
- 54.88386, -2.82979
- Source
- Historic England listing
Description
Corby Bridge, also known locally as Wetheral Viaduct, was begun in 1830 and completed in 1834 by Francis Giles, with construction by William S. Denton for the Newcastle & Carlisle Railway Company. The bridge is made entirely of red sandstone, using facing stones from Newbiggin Quarry near Carlisle and rubble infill from Wetheral and Corby Beck Quarries. In 1851, a cast iron footbridge with a wooden plank walkway was added at the parapet level on the north face, engineered by P. Tate and contracted by C.D. Richardson.
The structure features two piers in the river bed and two on either bank, supporting five semicircular arches that span 27 meters each. These arches are constructed from large blocks of dressed stone with channelled joints and voussoirs. The parapet stands 1.5 meters high, contributing to a total height of 33 meters from the summer level of the river. The bridge is wide enough to accommodate double tracks and has a total length of 280 meters.
As a significant early railway viaduct, it serves as an important landscape feature in an area of outstanding natural beauty. Notable elements include a footbridge with a cast inscribed plate at the east end, foundation stones built into either side of the parapet at the west end, and a centrally placed stone inscribed with the names of the engineer and builder. There are also N.E.R. gas lamp brackets at both the west end and the center of the footbridge, although the lamps are missing, along with railings on the parapet of the south side.
Local climate
Corby Bridge sits in a wetter-than-average part of the UK, with an average of 1,090 mm of rain a year. This makes it wetter than 87% of listed buildings in the UK. Its exposure to wind-driven rain is greater than that of 79% of listed buildings.
It experiences an average of 54 freeze-thaw cycles a year, more than 95% of listed buildings. Of these, 29 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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- Church of the Holy Trinity and St Constantine