Watersheddles Reservoir | |
---|---|
Water Sheddles | |
Location | Borough of Pendle, Lancashire |
Coordinates | 53°50′20″N2°03′04″W / 53.8390°N 2.0512°W Coordinates: 53°50′20″N2°03′04″W / 53.8390°N 2.0512°W |
Type | Reservoir |
Primary outflows | River Worth |
Catchment area | 560 acres (225 ha) |
Basin countries | England |
Managing agency | Yorkshire Water |
Built | 1871–1877 |
First flooded | 1877 |
Surface area | 27 acres (11 ha) |
Average depth | 18 feet (5.5 m) |
Max. depth | 49 feet (15 m) |
Water volume | 28,300,000 cubic feet (801,000 m3) |
Shore length1 | 1.2 miles (2 km) |
Surface elevation | 1,099 feet (335 m) |
References | [1] |
1 Shore length is not a well-defined measure. |
Watersheddles Reservoir is an upland artificial lake in Lancashire, England. The reservoir was opened in 1877 by the Keighley Corporation Water Works, and is now owned by Yorkshire Water. It supplies water to the Worth Valley and Keighley area and compounds several streams at the source of the River Worth.
Although the reservoir is just across the boundary of Lancashire, all of the water is used in the West Yorkshire region.
Due to the peatland in the immediate catchment area, the reservoir is prone to a high acidity and discolouration in its water.
The building of the three reservoirs in the Upper Worth Valley (Watersheddles, Ponden and Lower Laithe), was so that the Keighley area could have a supply of fresh drinking water, and also in response to several droughts in the 1860s. These droughts forced residents in the Upper Worth Valley to raid mill-ponds for drinking water. [2]
In response to the flooding, and as part of their endeavour to improve the water supply in Keighley and its environs, the Keighley Waterworks Extension and Improvement Act (1869) was passed to allow them to build "...an aqueduct, conduit, or watercourse commencing in the hamlet or liberty of Oakworth, in the township and parish of Keighley, in the said West Riding, at a point situate upon the stream called White Reaps Clough, distant 132 yards, or thereabouts, from the junction of the said stream with another stream called Dean Clough, and terminating in the northern side of the intended Water Sheddles Reservoir (proposed to be constructed by the Local Board under the powers of "The Keighley Waterworks Extension and Improvement Act, 1869 ") at a point 35 yards to the south of another point 320 yards distant (measured along the highway next hereinafter mentioned) from the Standing Stone on the boundary between the counties of York and Lancaster, such stone being placed on the highway leading from Keighley to Colne, such termination being in the hamlet of Wycoller...." [3]
So although the reservoir would dam the River Worth, it would be located 100 yards (91 m) over the county boundary in Lancashire, [4] a situation that still exists today, with the reservoir in the Borough of Pendle, but with a Bradford (BD) postcode. [5] The reservoir needed to be quite elevated in comparison to the town of Keighley, so that the water pressure would be sufficient to pump water to the uppermost areas of the town and adjoining localities. [6]
The name, which is recorded both as Watersheddles and Water Sheddles, is thought to have derived from Middle English meaning "the parting of the waters". [7] The name is borrowed from a nearby boundary stone on the road between Stanbury and Laneshaw Bridge. [8] [9] [10] [note 1]
Although the contract for the building of the reservoir was awarded to Walker and Taylor of Crewe in June 1870, [12] the reservoir was not started until August 1871, with full use and final flooding in 1877. [13] [note 2] [14] A deal was agreed with the mill owners along the River Worth that guaranteed a ready-supply of water; every morning and every evening, the sluices were opened to allow a regulated flow of water down the valley to enable the mills to restock their ponds. [15] [16] Keighley Corporation Water Works operated the reservoir until 1959, when it was folded into the newly created Craven Water Board (CWB). [17] The CWB, itself, was subsumed into Yorkshire Water in 1974. [18] [19] Whilst Yorkshire Water own the reservoir, unlike other reservoirs nearby that are in West Yorkshire, they do not own the surrounding land which drains into Watersheddles. [20]
Due to its location and the surrounding topography, the overflow channel is very steep (1 in 2.5) [21] and the length of spillway is 330 feet (100 m) long, with the width being 11 feet (3.5 m). [22] The dam height is 72 feet (22 m) and the dam wall stretches for 132 yards (121 m). [12] [14]
The maximum capacity of the reservoir is 191,000,000 imperial gallons; 229,000,000 US gallons (867,000,000 L), (28,300,000 cubic feet (801,000 m3)), and, along with Keighley Moor Reservoir, supplies 5% of its maximum volume on a daily basis for drinking water. [1] [23] [24] The reservoir is located some 3 miles (4.8 km) west of Stanbury and at an elevation of 1,099 feet (335 m). It has a maximum depth of 49 feet (15 m), an average depth of 18 feet (5.5 m) and has a catchment area of 560 acres (225 ha). [25] The short-distance path the Brontë Way, runs alongside the northern edge of the reservoir. [26]
Water from the reservoir is sent to a water treatment works (WTW) at Oldfield on the north side of the Worth Valley. Oldfield WTW also receives water from Keighley Moor Reservoir, and between the two, they supply over 1,800,000 imperial gallons; 2,100,000 US gallons (8,000,000 L) per day. [27] Oldfield was opened in 1891 in an effort to treat the water from the reservoirs as the acidic water was eating into the pipes and poisoning the water with lead. [24] A report from 1897 relays how the water is cleared through limestone, coke, sand and "polarite", [note 3] but suffered from discolouration arising from peat sediment settling on the bottom of the reservoir. [28] In 1973, just before Yorkshire Water assumed control of Watersheddles and Oldfield WTW, the pH of water arriving at Oldfield was registered as being between 6.9 and 7.0. [29]
The waters entering the reservoir drain a peat moorland with millstone grit underlying. The water was recorded with a pH value of 4.1 in 1988 and has been noted for its 'colour', which takes a more intensive process to remedy at the WTW. [25] [27] The problems of the pH value at Watersheddles (and to an extent, Keighley Moor Reservoir) were so bad, that Yorkshire Water designed and built their own prototype triple-pH controller in 1988 to regulate the waters acidity. [31]
In the late 1890s and early 1900s, a rain gauge was sited at Watersheddles, the results of which are given below;
Year | Rainfall | Ref | Year | Rainfall | Ref | Year | Rainfall | Ref |
---|---|---|---|---|---|---|---|---|
1897 | 49.83 inches (1,266 mm) | [32] | 1904 | 46.36 inches (1,178 mm) | [33] | 1908 | 50.6 inches (1,290 mm) | [34] |
1898 | 44.53 inches (1,131 mm) | [35] | 1906 | 54.33 inches (1,380 mm) | [36] | 1911 | 36.49 inches (927 mm) | [37] |
1900 | 51.73 inches (1,314 mm) | [38] | 1907 | 55.57 inches (1,411 mm) | [39] | 1913 | 45.35 inches (1,152 mm) | [40] |
The water at the reservoir between 2013 and 2016 was assessed as moderate for ecological quality and good for chemical quality. [41]
Haworth is a village in the City of Bradford, West Yorkshire, England, in the Pennines, 3 miles (5 km) south-west of Keighley, 10 miles (16 km) west of Bradford and 10 miles (16 km) east of Colne in Lancashire. The surrounding areas include Oakworth and Oxenhope. Nearby villages include Cross Roads, Stanbury and Lumbfoot.
Oxenhope is a village and civil parish near Keighley in the metropolitan borough of Bradford, West Yorkshire, England. The population was 2,476 at the time of the 2001 census which had increased to 2,626 at the 2011 Census. Historically part of the West Riding of Yorkshire, Oxenhope railway station is the terminus for the Keighley and Worth Valley Railway.
Keighley is a market town and a civil parish in the City of Bradford Borough of West Yorkshire, England. It is the second largest settlement in the borough, after Bradford.
Stanbury is a village in the Haworth, Cross Roads and Stanbury civil parish, and in the metropolitan borough of the City of Bradford in West Yorkshire, England. The name Stanbury translates as Stone Fort from Old English.
The River Worth is a river in West Yorkshire, England. It flows from minor tributaries on the moors above Watersheddles Reservoir down the Worth Valley to Haworth, where it is joined by Bridgehouse Beck which flows from Oxenhope. The River Worth is itself a tributary of the River Aire, which it joins at the end of the Worth Valley in Keighley.
Worth Valley is a ward in the City of Bradford Metropolitan District Council, West Yorkshire. The population of the ward taken at the 2011 Census was 14,387. It is named after the River Worth that runs through the valley to the town of Keighley where it joins the River Aire. In the north it is bounded by North Yorkshire, in the west by Lancashire and in the south by Calderdale District.
Yorkshire Water is a water supply and treatment utility company servicing West Yorkshire, South Yorkshire, the East Riding of Yorkshire, part of North Lincolnshire, most of North Yorkshire and part of Derbyshire, in England. The company has its origins in the Yorkshire Water Authority, one of ten regional water authorities created by the Water Act 1973, and privatised under the terms of the Water Act 1989, when Yorkshire Water plc, the parent company of the Yorkshire Water business, was floated on the London Stock Exchange. The parent company was Kelda Group in 1999. In February 2008, Kelda Group was bought by a consortium of infrastructure funds.
Oldfield is a small hamlet within the county of West Yorkshire, England, situated north of Stanbury and near to Oakworth. It is approximately 6 miles (9.2 km) west of the town of Keighley. It mainly consists of farmland and has panoramic views across the Worth Valley towards Brontë Country. Top Withens, the house featured in the novel Wuthering Heights, is clearly visible.
Dale Dike Reservoir or Dale Dyke Reservoir is a reservoir in the north-east Peak District, in the City of Sheffield, South Yorkshire, England, a mile (1.6 km) west of Bradfield and eight miles (13 km) from the centre of Sheffield, on the Dale Dike, a tributary of the River Loxley.
Thornton Steward Reservoir is a reservoir north of the village of Thornton Steward in North Yorkshire, England. It is owned by Yorkshire Water, and supplies drinking water to Swaledale, Wensleydale, Northallerton, and Thirsk.
The South Pennines is a region of moorland and hill country in northern England lying towards the southern end of the Pennines. In the west it includes the Rossendale Valley and the West Pennine Moors. It is bounded by the Greater Manchester conurbation in the west and the Bowland Fells and Yorkshire Dales to the north. To the east it is fringed by the towns of West Yorkshire whilst to the south it is bounded by the Peak District. The rural South Pennine Moors constitutes both a Site of Special Scientific Interest and Special Area of Conservation.
Cross Roads with Lees or Cross Roads cum Lees is a village in the Haworth, Cross Roads and Stanbury civil parish within the City of Bradford Metropolitan District, West Yorkshire, England. Historically part of the West Riding of Yorkshire, it lies less than 1-mile (1.6 km) from Haworth, approximately 2.5 miles (4 km) from Keighley and approximately 9 miles (14 km) from Bradford.
Baitings Reservoir is a large water supply reservoir operated by Yorkshire Water close to Ripponden in the West Yorkshire Pennines, England. It lies in the valley of the River Ryburn and is the higher of two reservoirs built to supply Wakefield with water and was completed in 1956. The lower reservoir is Ryburn Reservoir.
Essex and Suffolk Water is a water supply company in the United Kingdom. It operates in two geographically distinct areas, one serving parts of Norfolk and Suffolk, and the other serving parts of Essex and Greater London. The total population served is 1.8 million. Essex and Suffolk is a 'water only' supplier, with sewerage services provided by Anglian Water and Thames Water within its areas of supply. It is part of the Northumbrian Water Group.
Lower Laithe Reservoir is a man-made upland reservoir that lies 1.2 miles (2 km) west of Haworth, West Yorkshire, England. The reservoir was initially approved under the Keighley Waterworks and Improvement Act of 1869 but work did not begin on its construction until 1911 and even then was delayed because of the First World War. The reservoir was officially opened in August 1925 in front of a crowd of over 8,000 people. Its final tally on cost was £500,000. The reservoir lies in the Sladen Valley and was often referred to as Sladen Valley Reservoir.
Penistone Hill Country Park is an open space of moorland that is located to 0.31 miles (0.5 km) west of Haworth and 0.62 miles (1 km) north-west of Oxenhope in West Yorkshire, England. The park's highest point is detailed with a trig point which is 1,030 feet (310 m) above sea level. Since 1994, the park has been notified as being an SSSI as part of the South Pennine Moors.
Hainworth is a hamlet 1 mile (2 km) south of Keighley in West Yorkshire, England. The hamlet faces north across the lower end of the Worth Valley with a steep wooded incline towards Keighley.
Ponden Reservoir is an artificial upland lake in the Worth Valley, near Stanbury, West Yorkshire, England. Ponden was built as a compensation reservoir after the nearby Watersheddles Reservoir (upstream) was used to divert water away from the River Worth. Ponden was needed to regulate the flow of water down the river into the downstream mills in the valley.
The Worth Valley is a geographic area in West Yorkshire, England, that extends eastwards from Crow Hill and Oxenhope Moor, providing drainage for the River Worth for nearly 10 miles (16 km) to the River Aire. It is a side valley to Airedale, with the River Worth being a major tributary of the River Aire. The Worth Valley was important for its contribution to the textiles industry of the West Riding of Yorkshire and was furnished with several reservoirs to allow mills to operate within the valley. Most of the reservoirs are still in use into the modern day.
Upper Barden Reservoir is an upland fresh water reservoir, one of two reservoirs that collect water from Barden Moor, and dam Barden Beck, a tributary of the River Wharfe in the Yorkshire Dales, North Yorkshire, England. The reservoir was opened in 1882 and also supplies fresh water to the Nidd Aqueduct, which transports it to Bradford. Upper Barden Reservoir was the second of the reservoirs to be built,.