River Douglas, Lancashire facts for kids

Quick facts for kids Douglas
River Douglas at Appley Bridge, West Lancashire
Country	England
Physical characteristics
Main source	Winter Hill
River mouth	confluence with River Ribble 53°44′4.92″N 2°51′18.26″W / 53.7347000°N 2.8550722°W / 53.7347000; -2.8550722
Length	56 km (35 mi)
Basin features
Tributaries	Right: River Yarrow

The River Douglas, also known as the River Asland or Astland, is a river that flows through the Lancashire region, being found in the ceremonial counties of Lancashire and Greater Manchester in the north-west of England. It is a tributary of the River Ribble and has itself several tributaries, the major ones being the River Tawd and the River Yarrow.

In 1720 an act of Parliament was passed allowing Thomas Steers and William Squire to make the Douglas navigable to small ships between Wigan and its mouth. Amid financial irregularities, the Douglas Navigation was not completed until 1742, and by 1783, it had been superseded by the Leeds and Liverpool Canal. It reverted to being a river, although the remains of several locks can still be seen between Parbold and Gathurst. The Rufford Branch of the canal joins the river at Tarleton. The river rises on Winter Hill on the West Pennine Moors, and flows for 35 miles (56 km) through several towns and onto the Ribble estuary past Tarleton, the last 10 miles (16 km) or so being tidal. In 1892 the Douglas was diverted in Wigan to allow the construction of Wigan Central railway station.

Etymology

The Douglas is derived from the Brittonic elements dūβ-, meaning "black", and *glẹ:ss, "stream, rivulet, watercourse" (Welsh du-glais). This etymology is shared by like-named rivers in The Old North, such as the Douglas Water in Scotland.

Route

The River Dougles rises as a series of springs on Rivington Moor, close to the 1,440-foot (440 m) contour and near to the summit of Winter Hill. They are called Douglas Springs, and the River Yarrow, one of its major tributaries, rises at more springs less than a mile (1.6 km) to the north-west. Nearby are Anglezarke Reservoir, Upper Rivington Reservoir, and Lower Rivington Reservoir, three reservoirs that form part of the Rivington Chain, a network of reservoirs built to meet the drinking water needs of Liverpool. These disrupt the natural drainage patterns of both rivers.

The Douglas descends rapidly, dropping below the 430-foot (130 m) contour before it empties into the bottom end of Lower Rivington Reservoir, just to the north of Horwich. Below the dam, flow in the river is maintained by compensation water released from the reservoir, and marks the county boundary between Greater Manchester and Lancashire. It is crossed by the M61 motorway near Rivington services, and then turns to the north-west to reach the southern edge of Adlington. As it weaves its way in a generally south-westerly direction, it is crossed by the Leeds and Liverpool Canal, carried on a grade II listed aqueduct designed by John Rennie in the 1790s. It has a round arch and is constructed of rock-faced stone. Next, it enter Worthington Lakes, a series of three reservoirs built in the 1860s to provide drinking water for Wigan, and now managed as a country park by United Utilities. The river ceases to form the country boundary just before the lakes, and re-emerges from a tunnel below the reservoir dam, passing to the east of Standish. It continues southwards to Wigan, where it passes through a long culvert under the railway near Wigan North Western station, is crossed again by the Leeds and Liverpool Canal, and heads north-west, closely paralleled by the canal.

The River Douglas passing under Tarleton Bridge at Tarleton.

It is crossed by the M6 motorway and the Manchester-Southport line near Gathurst station, passes by the village of Appley Bridge, and at Parbold the canal crosses for the third time, as the river turns to the north and north-west. The aqueduct was designed by John Longbotham, has a semi-elliptical arch, and dates from 1791-2. The river drops below the 33-foot (10 m) contour at Parbold, and continues across open countryside where it is joined by the River Tawd, flowing north from Skelmersdale, becoming tidal before it reaches the village of Rufford. White Bridge at Rufford is a grade II listed structure with three spans, constructed of squared sandstone. It carries the B5246 Station Road over the river, and dates from the time of the construction of the Douglas Navigation, between 1720 and 1742. Below the bridge, the channel is rather straighter. Until 1805, the river was joined by the Rufford Branch of the Leeds and Liverpool Canal at Sollom Lock, but the lock was abandoned and a new one built further downstream at Tarleton. In order to do this, a new channel was created for the river further to the east, and the original channel was reused by the canal. On the new section, Great Hanging Bridge is similar to White bridge, both in date and in its three arches, and it carries the A581 road. Below it, the river is joined by the River Yarrow, which has taken a more direct route from its source to this point. At Tarleton, another three-span bridge carries the A59 road over the river. It is built from rock-faced sandstone blocks, and the keystone on the southern side indicates it was constructed in 1821. The north side is of red sandstone, with indications that it might once have been part of a narrower bridge. After its junction with the canal at Tarleton Lock, the final 4 miles (6.4 km) of the river to its junction with the River Ribble, here also known as the River Asland, is used by boat traffic transferring from the Leeds and Liverpool Canal to the Lancaster Canal since the opening of the Ribble Link in 2002.

Hydrology

The reservoirs of the Rivington Chain capture and store run-off from Winter Hill and Rivington Moor, much of which is used to provide a public water supply to areas of Lancashire and Greater Manchester. However, as a result of the original statutes that allowed them to be built, the water company is required to maintain some flow in the river below the reservoirs, and this compensation flow provides a fairly steady baseline flow in the river throughout the year. It is only normally exceeded if the reservoirs become full. On the upper reaches of the Douglas, the river bed is relatively steep, and consequently the river level can change quickly as a result of rainfall. As the river progresses to the west, the gradient lessens, and level changes occur more slowly.

There are two locations on the river where water is abstracted to maintain levels in the Leeds and Liverpool Canal. On many sections of the river, flows are augmented by the discharge from sewage treatment works. Major treatment works are located at Horwich on the upper river, at Wigan Wastewater Treatment works in Lathom on the central section, and at Skelmersdale on the River Tawd. Upgrades to the Wigan and Skelmersdale Treatment Works have been carried out, to improve the quality of the final effluent before discharge into the river system, while in Wigan, the sewage system has been improved, to reduce the amount of raw sewage discharged into the river by combined sewer overflows. In Standish, the pumping station at Chorley Road has been upgraded to reduce its impact on the river, while in Horwich, there was an ongoing scheme in 2014 in which volunteers walked the river to identify pollution points, which were then followed up by officers from the Environment Agency. Run-off of nutrients and other pollutants from agricultural land has also been addressed through the Catchment Sensitive Farming project, run jointly by Natural England, the Environment Agency and the Department for Environment, Food and Rural Affairs. Another joint initiative between the Environment Agency and the Royal Society for the Protection of Birds has seen sea defences improved and 370 acres (150 ha) of saltmarsh created as part of the Hesketh Outmarsh Coastal Realignment project.

Tributaries

River Douglas from the gardens at Bank Hall.

• Longton Brook
• Centre Drain
• Carr Heys Watercourse
• Tarra Carr Gutter
  • Hall Pool
• Dunkirk Dib
• Rakes Brook
• Carr Brook
• Strine Brook
• River Yarrow
  • tributaries of the Yarrow listed under River Yarrow

Water quality

The Environment Agency measure the water quality of the river systems in England. Each is given an overall ecological status, which may be one of five levels: high, good, moderate, poor and bad. There are several components that are used to determine this, including biological status, which looks at the quantity and varieties of invertebrates, angiosperms and fish, and chemical status, which compares the concentrations of various chemicals against known safe concentrations. Chemical status is rated good or fail.

The water quality of the River Douglas system was as follows in 2016. The section marked Ribble covers the tidal River Ribble and the lower 4 miles (6.4 km) of tidal River Douglas. Reasons for the quality being less than good include sewage discharge for most of the river, together with physical modification of the channel and poor nutrient management of agricultural land on the lower sections.