Dutton Railway Viaduct is a Grade II* listed building in the Cheshire West and Chester local planning authority area, England. First listed on 18 July 1986. Railway viaduct.

Dutton Railway Viaduct

WRENN ID
frozen-lancet-ochre
Grade
II*
Local Planning Authority
Cheshire West and Chester
Constituency
Chester South and Eddisbury MP: Aphra Brandreth (Con)
Country
England
Date first listed
18 July 1986
Type
Railway viaduct
Address
Dutton Railway Viaduct, Weaver Navigation, Acton Bridge
OS grid reference
SJ 582 763
Coordinates
53.28256, -2.62805
Source
Historic England listing

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

Description

Dutton Railway Viaduct is a railway viaduct completed in 1836 by Joseph Locke and George Stephenson for the Grand Junction Railway Company. It is constructed from rock-faced red sandstone with ashlar dressings and features 20 deep segmental arches made up of 40 voussoirs. Each arch has a dropped ashlar keystone and rests on concavely battered piers consisting of 16 cyclopean courses on plain plinths. The viaduct includes simple battered pilasters on each rectangular plinth at the outer cornice and has projecting copings. There are cutwaters to the piers of two arches, which are now dry, adjacent to the River Weaver, following the re-alignment of the Weaver Navigation. Steel pylons from the 1960s were added for electrification.

Dutton Viaduct is the longest on the Grand Junction Railway and is an early example of a major railway viaduct, displaying more assurance than the earlier Sankey Viaduct on the Liverpool and Manchester Railway, which was built by the same engineers just three years prior. The construction cost was £54,440, with McIntosh of London as the contractor. Notably, no lives were lost and no serious injuries occurred during its construction, leading to a civic celebration upon its completion.

Local climate

Dutton Railway Viaduct receives an average of 950 mm of rain a year. This makes it wetter than 74% of listed buildings in the UK. Its exposure to wind-driven rain is lower than that of 55% of listed buildings.

It experiences an average of 38 freeze-thaw cycles a year, more than 73% of listed buildings. Of these, 20 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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