Ouse Valley Railway Viaduct the Ouse Valley Railway Viaduct is a Grade II* listed building in the Mid Sussex local planning authority area, England. First listed on 11 May 1983. Viaduct.

Ouse Valley Railway Viaduct the Ouse Valley Railway Viaduct

WRENN ID
buried-terrace-ebony
Grade
II*
Local Planning Authority
Mid Sussex
Constituency
East Grinstead and Uckfield MP: Mims Davies (Con)
Country
England
Date first listed
11 May 1983
Type
Viaduct
Address
Ouse Valley Railway Viaduct the Ouse Valley Railway Viaduct, Balcombe
OS grid reference
TQ 322 279
Coordinates
51.03571, -0.11499
Source
Historic England listing

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

Description

The Ouse Valley Railway Viaduct is a significant structure located partly in the Parish of Cuckfield Rural. It is a remarkable example of scenic design and is the most important surviving architectural feature of the original layout of the London to Brighton Railway. Designed by John Rastrick and David Mocatta, the viaduct was constructed between 1839 and 1841. It is made of red brick and features 37 tall round-headed arches. Each pier is divided into two sections with a round-headed arch between them and a cornice above, situated below the springing of the main arch. At the top, there is a stone balustraded parapet with narrow round-headed arches and a small square recess over each pier, which projects out on brackets. At both ends of the viaduct, where it connects to the embankment, there are four solid rectangular brick piers topped with small pavilions that have a solid balustrade, three round-headed arches, a modillion eaves cornice, and a nipped tiled roof. These features serve as prominent terminal points of the viaduct, especially visible from passing trains. Sir John Rennie was the chief engineer for the railway line.

Local climate

Ouse Valley Railway Viaduct the Ouse Valley Railway Viaduct receives an average of 770 mm of rain a year. This makes it drier than 64% of listed buildings in the UK. Its exposure to wind-driven rain is greater than that of 67% of listed buildings.

It experiences an average of 31 freeze-thaw cycles a year, fewer than 63% of listed buildings. Of these, 13 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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