World Library  
Flag as Inappropriate
Email this Article

River Perry, Shropshire

Article Id: WHEBN0001919978
Reproduction Date:

Title: River Perry, Shropshire  
Author: World Heritage Encyclopedia
Language: English
Subject: Hordley, Shropshire, Ruyton-XI-Towns, Perry (disambiguation), Bagley, Shropshire
Publisher: World Heritage Encyclopedia

River Perry, Shropshire

River Perry
The river to the south of Mytton Bridge, just before it joins the River Severn
Origin Springs near Gobowen
Mouth River Severn, near Shrewsbury
Basin countries England
Length 24 miles (39 km)
Source elevation 850 feet (260 m)
Mouth elevation 200 feet (60 m)

The River Perry is a river in Shropshire, England. It rises near Oswestry and flows south to meet the River Severn above Shrewsbury. The channel has been heavily engineered, both to enable water mills to be powered by it, and to improve the drainage of the surrounding land. The middle section crosses Baggy Moor, where major improvements were made in 1777 to drain the moor, and a section of the river bed was lowered in the 1980s, to continue the process. The river was the scene of a major pollution incident in 1985, when pig slurry discharged into it, killing around 100,000 fish.


  • Route 1
  • Hydrology 2
  • Milling 3
  • Points of interest 4
  • Bibliography 5
    • References 5.1


The river rises as a series of springs near Hengoed, to the west of Gobowen and to the north of Oswestry, close to the 500-foot (150 m) contour. It passes under the Shrewsbury to Ruabon railway line and the A5 road, to skirt around the northern edge of Gobowen. It is joined by several other streams, which also rise at springs to the west of Gobowen, some from as high as 850 feet (260 m) above sea level, and another which rises near New Marton, and flows south, passing under the Llangollen Canal.

Passing under the A495 road to the north of Whittington, it enters the parkland of Halston Hall, supplying a large ornamental lake.[1] The hall is a red-brick country house, originally built in the 1690s, but altered for its owner John Mytton by Robert Mylne between 1766 and 1768. It is a grade I listed structure.[2] The river briefly heads south to leave the park, and then turns to the east, where it is crossed by the Montgomery Canal. At this point it is below the 260-foot (80 m) contour.[1] The Perry aqueduct, which carries the canal over the river, was the scene of a major breach in 1936, which led to the canal closing.[3] It was not reopened until 1987.[4]

Next it turns to the south, passing through Baggy Moor, where it is joined by a large number of drainage ditches. The railway line crosses it again, before it reaches Ruyton-XI-Towns, where there is a large loop around higher ground to the east.[1] The river is crossed by Platt Mill Bridge, designed and built in 1791 by Edward Cureton. The river forms the border between civil parishes at this point, and so one half of the bridge is in Ruyton-XI-Towns, while the other is in Baschurch. The bridge has two arches, and is a grade II listed structure.[5] A circular toll-house, built of red sandstone with a conical slate roof, was erected in the late eighteenth or early nineteenth century close to the bridge, and is now used as a house.[6] Continuing to the south-west of Baschurch, Milford Bridge is another two-arched structure, which carries the Baschurch to Little Ness road over the river. It was designed by Thomas Stanton in 1831, and was built by Nathaniel Edwards. Stanton was the civil engineer Thomas Telford's deputy at the time, when Telford was the County Surveyor of Bridges for Shropshire.[7] The river passes along the south-western edge of Yeaton Peverey parkland, to reach Forton Heath, where there is a bridge with a single elliptical arch, built in the early nineteenth century, which carries the Mytton to Forton road.[8] Below the bridge, the river joins the River Severn. The junction is not far from Shrewsbury, but the course of the Severn is much longer, as it flows around several large meanders to reach the town.[1]


The river rises on the edge of the North Shropshire sandstone plain, but for most of its length, the underlying rock is Bunter Sandstone.[9] A series of streams converge to the east of Gobowen, which have risen further to the west at heights of up to 850 feet (260 m).[10] Initially, the streams are stony-bottomed, but this is soon replaced by clays and alluvial silts. Near Rednal, the flow is augmented by the Tetchill Brook, which starts as an outflow from a large mere at Ellesmere. The outflow was a Victorian solution to control the levels of the mere. It is joined by Newnes Brook, which drains sandstone-based soils between Ellesmere and Gobowen. Below the junction the river crosses Baggy Moor, a large basin which was filled with peat, but which has been extensively drained to enable it to be used for agriculture.[9] Prior to 1777, it was flooded every winter, but an Act of Parliament was then obtained, to authorise the improvement and enclosure of 1,283 acres (519 ha) of land. This was one of the largest areas enclosed in north Shropshire, and although the scheme was more costly and difficult than enclosing some of the dryer areas, the resultant land was more fertile, and so justified the cost.[11]

Below the large meander at Ruyton, where a narrow valley cuts through sandstone, the bed flows over boulder clay with some glacial debris, and becomes stony again. The lower section retains some of its natural features, including meanders and riffle-pool sequences, which provide habitat for fish. Much of the upper section has been heavily modified, with the river canalised to improve flow. Between 1985 and 1988, the river bed between Ruyton and Rednal was lowered by about 3.4 feet (1.0 m), in order to improve the drainage of Baggy Moor.[9]

Water quality is affected by discharges from Sewage Treatment Plants, including one which reaches the river from Oswestry via the Common Brook, and another which discharged into the Tetchill Brook at Ellesmere prior to 1999.[9] The sewage works has since been closed, and improvements have been made to sewage outfalls and storm drains. In addition the brook has been dredged to remove polluted silts, and field studies have subsequently revealed that the quality of the brook is improving, measured by the diversity of invertebrates found in it.[12] In addition, water quality is affected by effluent from factories processing dairy products. These and the sewage works outfalls are generally well-regulated, but there have been some serious pollution incidents as a result of poor agricultural practice. The worst was in September 1985, when 50,000 imperial gallons (230 m3) of pig slurry was discharged into the river, resulting in the destruction of all of the fish populations down to the River Severn.[9] A tank containing the slurry burst, and around 100,000 fish died as a result of the pollution.[13]

Flow on the river is measured at three gauging stations. The furthest upstream is at Perry Farm, which uses a flat V triangular profile weir. That at Ruyton Bridge is a velocity area gauging station, while the final one is at Yeaton, where there is a Crump Profile weir. The catchment area above the Yeaton station is 69.8 square miles (180.8 km2), which receives a mean rainfall of 30.2 inches (767 mm). This results in a mean flow of 30.4 million gallons per day (138.2 Mld), although a peak flow of 336 million gallons per day (1528 Mld) was recorded in February 1990.[14]


The river has been modified significantly to power water mills over the centuries. The furthest upstream was probably at Rednal Mill, which is thought to be the site of a water mill, but showed no signs of a water management system in 1875, although there appears to be a bypass channel to the north, and the administrative boundaries do not follow the main channel at this point.[15][16] Between Ruyton and the River Severn, there were seven further corn mills, all of which are clearly marked on maps from 1880 to 1882.[17]

New Mills was just below Platt Bridge, while Milford Mill was just above Milford Bridge. Adcote Mill was by Adcote Farm, and most of the channels can still be seen. There were two mills at Yeaton, the Upper Mill and the Lower Mill, either side of Yeaton Bridge, and the final two were Fitz Mill and Mytton Mill.[17] Fitz Mill was operational between the twelfth century and 1926, and the structure is now used by a haulage company.[18] Mytton Mill was operational until 1966, when production ceased. The building was unused until 1971, when it became offices for a building contractor. A fire caused severe damage in 1982, but the building has since been restored, and now provides workshops for a number of small businesses, including the building contractor.[19]

Points of interest


  • Baugh, G C; Elrington, C R (1989). A History of the County of Shropshire: Volume 4: Agriculture. Victoria County History / British History Online. 
  • Harper, David M (1990). "The ecology of a lowland sandstone river: The River Perry, Shropshire" (PDF). Field Studies (Field Studies Council) (7). 
  • Jones, Dr. J. A. A. (1997). Global Hydrology. Prentice Hall.  
  • Marsh, Terry; Hannaford, Jamie (2008). UK Hydrometric Register (PDF). Natural Environment Research Council.  
  • Squires, Roger (2008). Britain's restored canals. Landmark Publishing.  


  1. ^ a b c d Ordnance Survey, 1:50,000 map
  2. ^  
  3. ^ Nicholson 2006, p. 65
  4. ^ Squires 2008, p. 123
  5. ^  
  6. ^  
  7. ^  
  8. ^  
  9. ^ a b c d e Harper 1990, pp. 453–454
  10. ^ Harper 1990, p. 455
  11. ^ Baugh & Elrington 1989, pp. 168–231
  12. ^ Holmes, David. "Freshwater pollution - a case tudy using the River Perry" (PDF). Geo Press.  
  13. ^ Jones 1997, p. 251
  14. ^ Marsh & Hannaford 2008, p. 69
  15. ^ Ordnance Survey, 1:2500 map, 1875
  16. ^ "Rednall Mill, SMRNO15588". Discovering Shropshire's History. Retrieved 2012-01-13. 
  17. ^ a b Ordnance Survey, 1:2500 map, 1880-1882
  18. ^ "Fitz Mill, SMRNO15595". Discovering Shropshire's History. Retrieved 2012-01-13. 
  19. ^ "Mytton Mill". BBC Domesday reloaded. Retrieved 2012-01-13. 
This article was sourced from Creative Commons Attribution-ShareAlike License; additional terms may apply. World Heritage Encyclopedia content is assembled from numerous content providers, Open Access Publishing, and in compliance with The Fair Access to Science and Technology Research Act (FASTR), Wikimedia Foundation, Inc., Public Library of Science, The Encyclopedia of Life, Open Book Publishers (OBP), PubMed, U.S. National Library of Medicine, National Center for Biotechnology Information, U.S. National Library of Medicine, National Institutes of Health (NIH), U.S. Department of Health & Human Services, and, which sources content from all federal, state, local, tribal, and territorial government publication portals (.gov, .mil, .edu). Funding for and content contributors is made possible from the U.S. Congress, E-Government Act of 2002.
Crowd sourced content that is contributed to World Heritage Encyclopedia is peer reviewed and edited by our editorial staff to ensure quality scholarly research articles.
By using this site, you agree to the Terms of Use and Privacy Policy. World Heritage Encyclopedia™ is a registered trademark of the World Public Library Association, a non-profit organization.

Copyright © World Library Foundation. All rights reserved. eBooks from Project Gutenberg are sponsored by the World Library Foundation,
a 501c(4) Member's Support Non-Profit Organization, and is NOT affiliated with any governmental agency or department.