River Dearne

River Dearne
The River Dearne viewed from the bridge behind Darton Post Office.
Origin	Birdsedge nr Denby Dale 53°33′52″N 1°42′37″W / 53.56444°N 1.71028°W / 53.56444; -1.71028
Mouth	River Don near Conisbrough 53°29′39″N 1°14′34″W / 53.49417°N 1.24278°W / 53.49417; -1.24278
Basin countries	England
Length	51.9 kilometres (32.2 mi)
Source elevation	328 metres (1,076 ft)
Mouth elevation	17 metres (56 ft)
Basin area	310.8 square kilometres (120.0 sq mi)

[ v t e ] River Dearne

Legend Dearne Head A629 road Park Dike A635 Barnsley Road Munchcliffe Beck Denby Dale railway station Thorpe Dike A626 road Kirklees Light Railway Park Gate Dike A626 road Bentley Brook Bretton Country Park Weirs A637 road M1 motorway (Jn 38) Cawthorne Dike Barnsley - Wakefield Railway A61 road, Barnsley A628 road, Barnsley A633 Grange Bridge Small Bridge Dike A635 Mill Houses Bridge River Dove A6195 road bridge Dearne Ings Bolton upon Dearne railway station New and Old channels Denaby Ings Nature Reserve River Don Navigation

The River Dearne is a river in South Yorkshire, England. It flows roughly east for more than 30 kilometres (19 mi), from its source just inside West Yorkshire, through Denby Dale, Clayton West, Darton, Barnsley, Darfield, Wath upon Dearne, Bolton on Dearne, Adwick upon Dearne and Mexborough to its confluence with the River Don at Conisbrough.

This was just one of many rivers that was involved in the 2007 United Kingdom floods.

The upper Dearne is followed by the Dearne Way, a footpath through the countryside from Dearne Head to Barnsley. The lower Dearne Valley is confusingly now also called Dearne Valley and is a regeneration area.

Attractions along the Dearne include the Yorkshire Sculpture Park at Bretton Hall, and Monk Bretton Priory.

The main tributary of the River Dearne is the River Dove.

Route

The river rises from just below the 330-metre (1,080 ft) contour to the west of Birdsedge. Within around 3 kilometres (1.9 mi), it reaches the A635 Barnsley Road bridge at Denby Dale, by which time it has dropped below the 175-metre (574 ft) contour, and its flow has been swelled by a number of springs and the output of the Park Dike. Below the bridge, the Munchcliffe Beck joins, and there is a large millpond, which supplied mills at Denby Dale. Beyond the mills, it crosses under a railway viaduct by Denby Dale railway station.^[1] The viaduct is curved, with 21 tall arches, and was built by the Lancashire and Yorkshire Railway in 1884.^[2] Next the river flows to the north east, with the A636 road closely following it on the north bank. It is joined by the Thorpe Dike at Kitchenroyd. It passes through Scissett and then to the west of Clayton West, where it is crossed by the Kirklees Light Railway. Park Gate Dike again swells the flow,^[1] before a double-arched skew bridge built in the early 19th century carries the A636 over the channel.^[3] Nearby is a hump-backed packhorse bridge with a single arch, probably built in the previous century,^[4] after which the river turns to the east to pass by the upper and lower lakes of Bretton Country Park on the south bank and Bretton Hall with the Yorkshire Sculpture Park on the north. There is a weir on the river and one on the outflow from the lakes, after which the 75-metre (246 ft) contour is crossed.^[1]

Next it turns to the south east and passes under the A637 road, the M1 motorway and the sliproads which form part of Junction 38, to reach Darton. The Cawthorne Dike joins from the west as it turns to the east and passes under the Wakefield to Barnsley railway line. The B6428 crosses on Barugh Bridge,^[1] a single span bridge made of rock-faced stone, which bears the date 1850 on the north-west buttress.^[5] As the river approaches Barnsley, the remains of the Barnsley Canal follow it on the south bank. Beyond the A61 Old Mill Lane bridge there was a mill, after which an aqueduct carried the canal over the river. Two more road bridges follow, the second of which carries the A633 Grange Lane.^[1] Just before the bridge is Priory Mill, a thirteenth-century mill which was heavily rebuilt by Sir William Armyne in 1635, and further remodelled in the nineteenth century. It was powered by a leat from the river, which supplied internal water wheels. Water from the leat was also channelled to Monk Bretton Priory, where it flushed the kitchens and the reredorter.^[6] Next there are two former railway bridges which now carry footpaths. Soon sections of the disused Dearne and Dove Canal run parallel to the river, and after passing under two more railway bridges, the course turns to the south to reach Darfield, below which the River Dove joins from the west. The river turns to the east again, passing to the north east of a series of lakes which form the Dearne Ings and Old Moor washlands.^[1] On the opposite side of the channel are the Bolton Ings washlands, which cover 110 acres (45 ha) and have been acquired by the Royal Society for the Protection of Birds (RSPB). In 2011, the site was in its early stages of development, but the reedbeds have attracted spoonbills and avocets, and are expected to act as a breeding ground for bitterns in due course.^[7] After the washlands, the river flows to the north of Wath upon Dearne, and to the south of Bolton on Dearne.^[1]

The railway to Bolton on Dearne station crosses, after which the river is flanked by the disused Bolton Common tip on the south bank. From the village of Adwick upon Dearne, which is a little further to the south, Harlington Road crosses the river at Adwick Bridge,^[1] a grade II listed twin-arched bridge built of sandstone around 1800.^[8] Denaby Ings nature reserve is separated from the river by a railway embankment on the north bank. The river sweeps round to the south to join the River Don just below Mexborough Low Lock, where Mexborough New Cut on the River Don Navigation rejoins the river.^[1] In 1903 the junction of the river with the Don was adjacent to the railway sidings of the Cadeby Main colliery,^[9] but by 1930 it had been moved further upstream, much closer to its present location.^[10]

Flood defences

The river regulator at Bolton upon Dearne may be removed as part of a flood risk management strategy.

By the 1950s, the course of the river near its mouth had been affected by subsidence from coal mining, and the lowering of the channel resulted in much of the surrounding land being regularly flooded. In order to alleviate the problem and restore the gradient of the channel at this point, a new channel was constructed on the south side of the railway embankment, from near Harlington to the River Don. The old channel can still be seen on the north side of the embankment, and connects to the Denaby Ings Nature Reserve.^[11]

As part of a comprehensive assessment of flood risks caused by the River Don and its tributaries, the River Dearne Improvement Scheme was implemented between 1963 and 1973. It was recognised that simple enlargement of the river channel would not provide a satisfactory solution, as it would just move the problem to the River Don, and therefore a series of washlands were created, which could be progressively flooded if required, without affecting centres of population. Near the mouth of the river, Dearne Mouth washland, which is now known as the Denaby Ings Nature Reserve, was created in 1963, and a manually operated sluice allowed the flow of the river to be diverted through the floodbank and into the washland when there were high levels at the junction with the River Don. The sluice was rebuilt in 1973. Additional washlands were created at Harlington and North Ings, and the river was straightened and realigned.^[12]

Further upriver, a flood relief channel was built at Bolton upon Dearne, and more washlands were formed between Wath railway bridge and Adwick bridge. The Bolton Ings and Old Moor washlands were next to be created, to be followed by those at Wombwell Ings, where the River Dove joins the Dearne, Darfield, Houghton and Cudworth. Some of the storage capacity was lost as a result of mining schemes, and a regulator was installed at Bolton in 1972, allowing the flow to be restricted by a sluice gate.^[13] During the flooding in 2007, all of the washlands filled to capacity, although the Bolton regulator could not be operated as it had been vandalised. Some damage to the Houghton washlands resulted from the extremely high water levels, which overtopped the banks and caused erosion to take place.^[14] Following the floods, a reassessment of the function of the regulators was carried out, and in view of the costs of maintaining them, the Environment Agency intend to remove them once some reconfiguration of the river channel has been completed. This work will ensure that the washlands fill and empty at the appropriate points in a flood cycle.^[15]

Water quality

In the late 1700s, the river held good populations of fish. Industrial development of the valley consisted of several deep coal mines, but they were fairly small, and did not significantly pollute the river. There were collieries at Smithies, Honeywell, Queens Ground and Mount Osborne. The opening of the Dearne and Dove Canal in 1810 had serious impacts on the river, as it provided a way to transport the coal to Sheffield and Rotherham, where it was used in the steelworks. This led to the rapid development of more and larger collieries. The population grew rapidly, but it was housed in small villages near the pits. With no urban infrastructure, sewage polluted the river, as did the industrial discharges from the mines.^[16]

Parts of the upper river were well suited to the woollen trade, and mills developed in the 19th century, at Denby Dale, Scissett and Clayton West. The valley of the upper river is quite narrow, and housing was provided by building terraces, which often backed on to the river. Again, sewage ended up in the river, as did the effluent from processing the wool, which included caustic washing agents and dyes. Water used in washing was returned to the river without adequate cooling, and the temperature rose. As early as 1896, the West Riding River Board was working hard to improve the situation, and achieved limited success by 1902, when they produced a report. They identified 44 small sewage treatment plants, none of which treated the sewage adequately, and noted that the river was "much polluted by domestic sewage and by untreated or partially treated trade refuse."^[17] By the early 1900s, the river was lifeless between Barnsley and the Don, with fish unable to survive in the cocktail of chemicals. The River Dove was also lifeless, although the Cawthorne Dyke and several other small tributaries managed to retain populations of brown trout.^[18]

The situation had not improved by the 1960s, when the Yorkshire Ouse River Board noted that industrial waste from the mining, paper making, brewing and textile industries was being dumping into the river without any treatment. Pressure from the Board and from local authorities based along the river resulted in some treatment being carried out, but by 1974 much of the river was still rated as Class E on the six-point water quality scale, which indicated it was of poor quality, with some parts rated as Class F, meaning that they grossly polluted with little or no life. Nevertheless, small pockets of fish began to appear. A small population of brown trout had survived in the upper 1.5 miles (2.4 km) of the river, but could not proceed downstream due to dams erected for the woollen mills. Moth-proofing agents were released by the mills into the water, which were highly toxic to fish, and although the discharge of these chemicals ceased in 1979, when they were routed to a sewer for treatment, the problem did not immediately go away, as the chemicals continued to seep into the river from land which had been contaminated by them for another ten years. Any progress with the re-establishment of fish stocks was destroyed by a series of releases of pollutants into the river during the 1970s and 1980s.^[19]

By 1987, water quality had improved sufficiently to try restocking the upper river, and large numbers of yearling trout were released into the river in April. A fish survey carried out by the Yorkshire Water Authority a year later showed that many of these were surviving. By 1992, there was evidence that the fish were breeding in the river, and naturally bred brown trout were found between Denby Dale and Clayton West in 1994, for the first time in over 100 years. The trout population in the upper Dearne was declared to be self-sustaining by 1996.^[20]

The river below Clayton West ceases to be a shallow, fast-flowing watercourse, and consists of deeper pools with a slower flow, which is suitable for various course fish as well as trout. By 1974, a modest improvement in water quality had been achieved by treatment of industrial effluent, and some fish managed to exist below the weir at the Star Paper Mill in Barnsley. The weir helped to oxygenate the water, and most of the fish had been washed downstream from Cannon Hall and Bretton Lakes. During flood conditions, many of the population would be washed further downstream, to be replaced by others from the lakes. A survey in 1982 found gudgeon, minnow and three-spined stickleback, which had increased by 1985, and over 10,000 course fish were released as part of a restocking programme. However, most of these were decimated by serious pollution incidents that affected the river in 1987 and 1988, and the incidents continued for a further three years. The sewage treatment works at Darton and Lundwood, on either side of Barnsley, were largely responsible.^[21]

Discharges from the Darton sewage treatment works contained residues from dyes used by a local carpet manufacturer, which reached the works by a foul sewer, but could not be adequately treated by the existing processes. As a result, the final effluent was a deep red colour, and were a major factor in the poor biochemical oxygen demand ratings for the river. Major improvements, including new primary settlement tanks and tertiary treatment lagoons, were made to the treatment works, and the carpet manufacturers installed facilities to treat their effluent before it was discharged to the sewer. By 1994, fish were again appearing below the Star Paper Mill weir, and Yorkshire Water and the Environment Agency carried out another fish restocking programme.^[22]

Improvements to water quality through Barnsley highlighted the fact that fish populations did not exist below the discharge from the Lundwood sewage treatment works to the east of Barnsley. As the population of Barnsley had increased, the volume of effluent received by the works had increased without a corresponding increase in its ability to treat it. In addition, the outfall reached the river along a 440-yard (400 m) stretch of the Cliffe Bridge Dyke, which had suffered from subsidence. This resulted in slow movement along the dyke, which sometimes caused the effluent to become septic before it reached the main channel. A major programme of refurbishment was carried out at the works between 1997 and 1998, to improve the quality of discharge. The fish populations on the lower river fluctuated, as a result of pollution incidents on the middle river, but by 1994, chub and dace were clearly breeding in the river. Breeding was assisted by re-engineering of the channel at Pastures Road, Denaby, which had been straightened in the 1960s after it was affected by subsidence. A series of bends were created, which encourage the formation of deep pools and shallow gravel riffles. These features are needed by dace and barbel for successful spawning, and prevent young fish from being washed downstream in flood conditions. Water quality has continued to improve, and the lower Dearne has become an important venue for angling.^[23]

Further improvements to the Lundwood sewage treatment works began in 2007 to enable it to comply with the Freshwater Fish Directive, and although the site was inundated during the floods of 2007, the scheme, which cost £8 million, was completed in 2008. To celebrate the opening of the new works, the poet Ian McMillan was asked to run a poetry workship at Littleworth Grange Primary Learning Centre, where children completed a poem about water treatment for which he supplied the first two lines.^[24][25]

Points of interest

See also

• Rivers of the United Kingdom

Bibliography

References