| Hurst Reservoir | |
|---|---|
 Hurst Reservoir before it was decommissioned | |
  Hurst Reservoir | |
| Location | North Derbyshire, England |
| Coordinates | 53°26′26″N1°55′00″W / 53.4406°N 1.9167°W Coordinates: 53°26′26″N1°55′00″W / 53.4406°N 1.9167°W |
| Type | impounding reservoir |
| Basin countries | United Kingdom |
Hurst Reservoir is a former, now disused, reservoir near Glossop, north Derbyshire.
In 1837, 50 local millowners and gentlemen, known as the "Glossop Commissioners", obtained an Act of Parliament to construct the Glossop Reservoirs. Hurst Reservoir was on the Hurst Brook and Mossy Lea Reservoir was to take water from the Shelf Brook. Only the Hurst Reservoir was constructed before the money ran out. Mossy Lea Reservoir was later constructed privately by the Duke of Norfolk. His engineer and surveyor was John Frederick Bateman. The reservoir was taken over in 1929 by the Glossop Corporation Waterworks. This became part of the Manchester Corporation Waterworks in 1959.
Swineshaw Reservoir, Hurst Reservoir, and Mossy Lea Reservoir are no longer in service. In 2013, the Hurst Reservoir embankment was removed and the silt that had built up over the previous 175 years was dispersed within the Hurst valley. The reservoir was decommissioned because it had not been used for drinking water for 25 years and maintenance of the dam could no longer be justified. Following the removal of the embankment, a small pond (fire break) was retained to benefit wildlife, with the stream being returned to its original course. [1] The former reservoir is next to Glossop & District Golf Club.
The River Etherow is a river in northern England, and a tributary of the River Goyt. Although now passing through South Yorkshire, Derbyshire and Greater Manchester, it historically formed the ancient county boundary between Cheshire and Derbyshire. The upper valley is known as Longdendale. The river has a watershed of approximately 30 square miles (78 km2), and the area an annual rainfall of 52.5 inches (1,330 mm).
The Great Sheffield Flood was a flood that devastated parts of Sheffield, England, on 11 March 1864, when the Dale Dyke Dam broke as its reservoir was being filled for the first time. At least 240 people died and more than 600 houses were damaged or destroyed by the flood. The immediate cause was a crack in the embankment, the cause of which was never determined. The dam's failure led to reforms in engineering practice, setting standards on specifics that needed to be met when constructing such large-scale structures. The dam was rebuilt in 1875.
Thomas Hawksley was an English civil engineer of the 19th century, particularly associated with early water supply and coal gas engineering projects. Hawksley was, with John Frederick Bateman, the leading British water engineer of the nineteenth century and was personally responsible for upwards of 150 water-supply schemes, in the British Isles and overseas.
Lake Vyrnwy is a reservoir in Powys, Wales, built in the 1880s for Liverpool Corporation Waterworks to supply Liverpool with fresh water. It flooded the head of the Vyrnwy valley and submerged the village of Llanwddyn.
Anglezarke Reservoir is the largest reservoir in the Rivington chain to the west of Anglezarke in Lancashire, England. Anglezarke Reservoir has three embankments: the Charnock Embankment, the longest, is 850 yards (777 m) long and 31 feet (9.45 m) high, the Knowsley Embankment is 240 yards (219.5 m) long and 45 feet (14 m) high and the Heapey Embankment is 280 feet (85.3 m) long and 32 feet (9.75 m) high. It is fed by the River Yarrow, which has been diverted from its original course which is now covered by the Knowsley Embankment. It served the city of Liverpool before its current status as a supply mainly for Wigan. The original `Rivington Pike Scheme' was undertaken by Thomas Hawksley between 1850 and 1857 for the Liverpool Corporation Waterworks. The scheme was to construct five reservoirs and a water treatment works at the south end of Lower Rivington with a 17-mile (27 km) pipeline to storage reservoirs at Prescot. Water from two higher level reservoirs, Rake Brook and Lower Roddlesworth, was carried south in `The Goit', a channel connecting them to the reservoirs.
Beacons Reservoir is the northernmost of the three reservoirs in the Taff Fawr valley in South Wales. It was built by Cardiff Corporation Waterworks between 1893 and 1897, and the water is impounded by an earth dam with a clay core. Since 1973 it has been owned by Welsh Water. As its name suggests, it is located in the Brecon Beacons National Park in the Powys unitary authority area and within the historic county boundaries of Breconshire.
Cantref Reservoir is the middle of the three reservoirs in the Taff Fawr valley in Wales. It was built by Cardiff Corporation Waterworks between 1886 and 1892, but since 1973 has been owned by Welsh Water. It is located in the Brecon Beacons National Park, mostly in the Powys unitary authority area and within the historic county boundaries of Breconshire. Part of the south west corner is in the Rhondda Cynon Taff unitary authority area.
Lower Rivington Reservoir is at the end of the Rivington chain of reservoirs in Lancashire, England, with Upper Rivington Reservoir to the north, and Rivington Water Treatment Works to the south. The Rivington chain primarily supplies 70,000 households in the Wigan area. The chain was built to supply Liverpool.
Woodhead reservoir is a man-made lake near the hamlet of Woodhead in Longdendale in north Derbyshire. It was constructed by John Frederick Bateman between 1847 and June 1877 as part of the Longdendale chain to supply water from the River Etherow to the urban areas of Greater Manchester. It is at the top of the chain of reservoirs and was the first to be started, though, due to construction problems, it was the last to be completed.
Arnfield Reservoir is a man-made lake in Longdendale in north Derbyshire. It was constructed in 1854 as part of the Longdendale chain to supply water from the River Etherow to the urban areas of Greater Manchester. Unlike the other reservoirs in the chain, Arnfield and Hollingworth Reservoir are not in the Etherow valley but lie in the valley of tributary brooks to the north and above. From Arnfield the water is extracted to pass through the Mottram Tunnel to Godley.
Lower Roddlesworth Reservoir is a reservoir on the River Roddlesworth close to Abbey Village in Lancashire, England.
Rake Brook Reservoir is a reservoir fed by two streams, including the eponymous Rake Brook, a tributary of the River Roddlesworth in Lancashire, England.
London's water supply infrastructure has developed over the centuries in line with the expansion of London. For much of London's history, private companies supplied fresh water to various parts of London from wells, the River Thames and the River Lea. Further demand prompted new conduits and sources, particularly when the Agricultural and Industrial Revolution caused a boom in London's population and housing.
Backwater Reservoir is a reservoir in north west Angus, Scotland. The reservoir's sole purpose is to provide drinking water, and as such, it supplies Angus, Dundee, and parts of Perth and Kinross. Backwater, together with the smaller Lintrathen Reservoir 4 kilometres (2.5 mi) to the south, is capable of supplying some 300,000 people with drinking water.
Worthington Lakes is a series of three reservoirs in Lancashire close to nearby Standish, off the A5106 Wigan to Chorley road in the north-west of England. They were constructed in the early 1860s to provide the clean water required by the rapidly growing town of Wigan.
For the reservoirs near Stalybridge, in Tameside, Greater Manchester, see Higher Swineshaw Reservoir and Lower Swineshaw Reservoir
Mossy Lea Reservoir is a disused reservoir near Glossop, north Derbyshire. In 1837, 50 local millowners and gentlemen, known as the "Glossop Commissioners", obtained an Act of Parliament to construct the Glossop Reservoirs. Hurst Reservoir was on the Hurst Brook and Mossy Lea Reservoir was to take water from the Shelf Brook. Only the Hurst Reservoir was constructed before the money ran out. Mossy Lea Reservoir was constructed privately in 1840 by the Duke of Norfolk. It was taken over in 1929 by the Glossop Corporation Waterworks. This became part of the Manchester Corporation Waterworks in 1959. Swineshaw Reservoir, Hurst Reservoir and Mossy Lea Reservoir are no longer in service.
Cardiff Corporation Waterworks, its predecessors and successors have provided a public water supply and sewerage and sewage treatment services to the Welsh city of Cardiff since 1850.
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.
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,.
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