Cound Brook
Cound Brook (pronounced COOnd) is a tributary of the River Severn in Shropshire, England, running to south of the county town Shrewsbury. The Cound Brook rises in the Stretton Hills and discharges into the River Severn at Eyton on Severn after winding its way for 25 miles (40 km) across the southern Shropshire-Severn plains.[1]
| Cound Brook | |
|---|---|
 Cound Brook viewed from Longnor Bridge | |
| Location | |
| Country | England |
| Region | West Midlands |
| County | Shropshire |
| Cities | Dorrington, Condover, Cantlop, Cound |
| Physical characteristics | |
| Source | |
| • location | All Stretton |
| • elevation | 176 m (577 ft) |
| Mouth | |
• location | River Severn, near Eyton on Severn |
• elevation | 41 m (135 ft) |
| Length | 40.5 km (25.2 mi) |
| Discharge | |
| • location | Eyton on Severn |
The flow of the Cound Brook can vary from sluggish in a dry summer to a raging torrent in winter or spring. The river is crossed by several bridges along its route including two historic and unusual iron bridges. Several other roads cross the river as fords. The river has breached its banks on the lower flood plain several times in the past and is now monitored by the local rivers authority.
The river is named after Cound, the last settlement it passes through prior to the confluence with the River Severn. Conversely one of the villages on its route, Condover, is thought to have been named after the river during the late medieval period.
The Coundmoor Brook is a smaller watercourse which flows into the Cound Brook near its confluence with the Severn at Cound.
Sources
The Cound rises from minor watercourses running off the Long Mynd and Caer Caradoc in the northern part of the "Stretton Gap", between the settlements of Church Stretton and All Stretton. One of the main initial tributaries is the stream that runs through the Carding Mill Valley, which is named "Ashbrook" as it flows through Church Stretton. In the village of All Stretton the Ashbrook combines with another considerable stream that comes down the Batch valley, effectively forming the beginning of the Cound, at grid reference SO461953. The embryonic river descends towards the Shropshire-Severn plain and heads north east mirroring the route of the A49 main road and the Shrewsbury to Hereford railway line.
Middle route
The brook passes to the east of Leebotwood and west of Longnor and the Medieval deer park there. Continuing to the east of Dorrington village, at Stapleton the Cound changes direction and heads eastwards.
The Cound passes through the historic and picturesque Condover with its conservation area and many Listed buildings. A water mill was recorded as standing on the Cound in Condover at the time of the Domesday Book. After Condover the river heads south east through Boreton.
Iron bridges
To the north of the village of Cantlop there is an unusual cast-iron single-span bridge known as the Cantlop Bridge, that was designed and constructed by Thomas Telford in 1818. Originally a road bridge to cross the Cound Brook, it now remains only as a historic monument as the original 19th century road route is now diverted alongside on a modern bridge.
The river then passes through the village of Cound and under another iron bridge, the Coundarbour bridge, also designed and built by Telford, the oldest iron bridge still in normal everyday use anywhere in the world and built in 1797. (Abraham Darby's famous Iron Bridge in Ironbridge, Telford, had closed to vehicular traffic in 1934 and is now only open to pedestrians.)
Discharge
The Cound Brook now follows an increasingly meandering route across a low lying flood plain until it discharges into the River Severn a few hundred yards west of Eyton on Severn and less than a mile south from Wroxeter (with its Roman city ruins), close to the northern end of the Watling Street Roman road from Dover.
References
- "Cound Brook". Catchment Data Explorer. Environment Agency. Retrieved 20 April 2016.