Chester Weir and Salmon Leap is a Grade I listed building in the Cheshire West and Chester local planning authority area, England. First listed on 23 July 1998. A Medieval Weir. 1 related planning application.
Chester Weir and Salmon Leap
- WRENN ID
- sheer-bronze-curlew
- Grade
- I
- Local Planning Authority
- Cheshire West and Chester
- Constituency
- Chester North and Neston MP: Samantha Dixon (Lab)
- Country
- England
- Date first listed
- 23 July 1998
- Type
- Weir
- Period
- Medieval
- OS grid reference
- SJ 407 658
- Coordinates
- 53.18625, -2.88788
- Source
- Historic England listing
Description
Chester Weir and Salmon Leap is a Grade I listed weir and former causeway across the River Dee, constructed in 1093 by Hugh Lupus, the first Earl of Chester, for St Werburgh's Benedictine Abbey, now known as the Cathedral Church of Christ & the Blessed Virgin Mary in Chester. The structure is made of sandstone and features a continuous weir with a sloping spillway composed of large rectangular stones. It measures 120 meters in length and is positioned at an acute angle to the riverbanks, with its north-west end running parallel to the bank for 33 meters. This design was intended to create the necessary head of water for the medieval Mills of Dee, which were built and expanded from 1093 to accommodate six mill-wheels and machinery by 1270. The stone salmon leap has been altered, and there is a leat for a later mill, also altered, located by the south bank. The mills on the north bank were demolished in 1910, while the one on the south bank was taken down around 1970. Historically, the Mills of Dee were among the largest and most valuable in England during the 13th century, generating an annual rental of 270 pounds. The weir was restored in the early 20th century to support the City Council's hydro-electric power station, which operated from 1913 to 1939 on the site of the former mills.
Local climate
Chester Weir and Salmon Leap receives an average of 890 mm of rain a year. This makes it wetter than 66% of listed buildings in the UK. Its exposure to wind-driven rain is lower than that of 78% of listed buildings.
It experiences an average of 31 freeze-thaw cycles a year, fewer than 62% of listed buildings. Of these, 14 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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- No EPC on record for this property
- No sale records on file
- Related listed building consents — 1 application
- 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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