Wessenden Head Reservoir | |
---|---|
Location | West Yorkshire |
Coordinates | 53°33′50″N1°53′46″W / 53.564°N 1.896°W |
Type | reservoir |
Primary inflows | Shiny Brook Loadley Clough stream |
Primary outflows | Wessenden Brook |
Basin countries | United Kingdom |
Built | 1881 |
Max. length | 0.3 kilometres (0.2 mi) |
Max. width | 300 metres (984 ft) |
Water volume | 372,780 cubic metres (82,000,000 imp gal) |
Surface elevation | 386 metres (1,266 ft) |
Wessenden Head Reservoir is the highest in a series of four reservoirs in the Wessenden Valley above the village of Marsden in West Yorkshire, at the northern end of the Peak District National Park. [1]
Following the Wessenden Act of Parliament of 1836, Wessenden Reservoir was created by the construction of an earth embankment across Wessenden Brook. The Huddersfield Waterworks and Improvements Act of 1876 approved the building of a new reservoir above Wessenden Reservoir. Wessenden Head Reservoir was built between 1877 and 1881, fed from a catchwater drain via a sluice in the Shiny Brook (a tributary of Wessenden Brook). The Huddersfield Waterworks Act of 1890 led to Huddersfield Corporation purchasing the reservoirs from the Wessenden Commissioners in order to supply drinking water to the town. [2] [3]
Wessenden Head Reservoir has a storage capacity of 82,000,000 imperial gallons (370,000,000 L). [2] The reservoir is currently owned and operated by Yorkshire Water.
The Wessenden Valley Woodland Project was initiated in 2017 to develop natural habitats with increased biodiversity. [4]
The Pennine Way long-distance footpath runs along the northern side of the reservoir and its dam. [1]
Meltham is a town and civil parish within the Metropolitan Borough of Kirklees, in West Yorkshire, England. It lies in the Holme Valley, below Wessenden Moor, 5 miles south-west of Huddersfield on the edge of the Peak District National Park. It had a population of 8,089 at the 2001 census, which was estimated to have increased to 8,600 by 2005. The population assessed at the 2011 Census was 8,534. It has 12 elected council members who meet up around every 6 weeks.
The Pennines, also known as the Pennine Chain or Pennine Hills, are a range of uplands mainly located in Northern England. Commonly described as the "backbone of England" because of its length and position, the range runs from Derbyshire and Staffordshire in the North Midlands to Northumberland in North East England, near the Anglo-Scottish border. The range starts near the valley of the River Trent to the south and extends northwards across the Peak District, South Pennines, Yorkshire Dales, and North Pennines, ending at the Tyne Gap. Beyond the gap are the Border Moors and Cheviot Hills, which are included in some definitions of the range.
The River Colne in West Yorkshire is formed at the confluence of two brooks that originate in the Pennines close to Marsden. It flows in an easterly direction through the Colne Valley and Huddersfield towards Cooper Bridge where it flows into the River Calder.
Dove Stone Reservoir lies at the convergence of the valleys of the Greenfield and Chew Brooks above the village of Greenfield, on Saddleworth Moor in Greater Manchester, England. The reservoir is on the western edge of the Peak District National Park. It supplies drinking water to the surrounding area and is a tourist attraction, providing several walks amongst picturesque landscapes.
Deanhead Reservoir is a reservoir near Scammonden, in the metropolitan district of Kirklees, West Yorkshire, England.
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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.
Marsden railway station serves the village of Marsden near Huddersfield in West Yorkshire, England. The station is on the Huddersfield Line, operated by Northern and is about 7 miles (11 km) west of Huddersfield station. It was opened in 1849 by the London & North Western Railway and is the last station before the West Yorkshire boundary with Greater Manchester. The station is operated by Northern Trains, but only Transpennine Express trains call here.
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Saddleworth Moor is a moorland in North West England. Reaching more than 1,312 feet (400 m) above sea level, it is in the Dark Peak area of the Peak District National Park. It is crossed by the A635 road and the Pennine Way passes to its eastern side.
The Wessenden Valley is a moorland valley in the Dark Peak, immediately south of Marsden in West Yorkshire, England. The name Wessenden derives from Old English and means the 'valley with rock suitable for whetstones'. The valley was formed by retreating glaciers at the end of the last ice age and continues to be cut by the Wessenden Brook a tributary of the River Colne with a catchment of 6.28 square miles (16.27 km2).
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.
Scammonden Reservoir is a water reservoir in West Yorkshire, England. Its water surface area when full is 42 hectares (0.16 sq mi). The level of the bellmouth overflow above sea level is 252 metres (827 ft). The reservoir holds 78,000,000,000 litres (1.7×1010 imp gal; 2.1×1010 US gal). Its length is 1.4 kilometres (0.9 mi).
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.
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Digley Reservoir is a lake located downstream of Bilberry Reservoir, 2 miles (3.2 km) south west of Holmfirth, in West Yorkshire, England. The reservoir was planned during the 1930s, with much land being bought for its construction, but it was not completed until 1954.
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Fernilee Reservoir is a drinking-water reservoir fed by the River Goyt in the Peak District National Park, within the county of Derbyshire and very close to the boundary with Cheshire. The village of Fernliee sits at the north end of the reservoir, with Goyt's Moss to the south and between Hoo Moor to the west and Combs Moss to the east.
Wessenden Reservoir is the second in a series of four reservoirs in the Wessenden Valley above the village of Marsden in West Yorkshire, at the northern end of the Peak District National Park.