Mossy Lea Reservoir | |
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Location | North Derbyshire, England |
Coordinates | 53°26′54″N1°54′51″W / 53.4483°N 1.9142°W Coordinates: 53°26′54″N1°54′51″W / 53.4483°N 1.9142°W |
Type | impounding reservoir |
Basin countries | United Kingdom |
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. [1]
Glossop is a market town in the Borough of High Peak, Derbyshire, England, 15 miles (24 km) east of Manchester, 24 miles (39 km) north-west of Sheffield and 32 miles (51 km) north of the county town, Matlock, near Derbyshire's borders with Cheshire, Greater Manchester, South Yorkshire and West Yorkshire. It is between 150 and 300 metres above mean sea level, and is bounded by the Peak District National Park to the south, east and north.
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).
Derwent Reservoir is the middle of three reservoirs in the Upper Derwent Valley in the north of Derbyshire, England. It lies approximately 10 miles (16 km) from Glossop and 10 miles (16 km) from Sheffield. The River Derwent flows first through Howden Reservoir, then Derwent Reservoir and finally through Ladybower Reservoir. Between them they provide practically all of Derbyshire's water, as well as to a large part of South Yorkshire and as far afield as Nottingham and Leicester.
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.
Bow Back Rivers or Stratford Back Rivers is a complex of waterways between Bow and Stratford in east London, England, which connect the River Lea to the River Thames. Starting in the twelfth century, works were carried out to drain Stratford Marshes and several of the waterways were constructed to power watermills. Bow Creek provided the final outfall to the Thames, and the other channels were called Abbey Creek, Channelsea River, City Mill River, Prescott Channel, Pudding Mill River, Saint Thomas Creek, Three Mills Back River, Three Mills Wall River and Waterworks River.
Bristol Water is a British water company which supplies 266 million litres of drinking water daily to over 1.2 million customers in a 2,600 km2 (1,000 sq mi) area centred on Bristol, England. It is regulated under the Water Industry Act 1991. Sewerage services in the Bristol area are provided by Wessex Water.
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.
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.
Molesey Lock is a lock on the River Thames in England at East Molesey, Surrey on the right bank.
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 in the three centuries after the construction in 1613 of the New River, the River Lea, which has springs that divert alongside Hertford at an elevation of 40 metres AOD. Further demand prompted new conduits and sources, particularly in the 150 years to 1900 as the Agricultural and Industrial Revolution caused a boom in London's population and housing.
The Lee Flood Relief Channel (FRC) is located in the Lea Valley and flows between Ware, Hertfordshire, and Stratford, east London. Work started on the channel in 1947 following major flooding and it was fully operational by 1976. The channel incorporates existing watercourses, lakes, and new channels. Water from the channel feeds the Lee Valley Reservoir Chain.
Dagenham Brook is a minor tributary of the River Lea located in the London Borough of Waltham Forest, and the traditional eastern limit of Leyton Marshes.
Whitfield is a hamlet in Derbyshire, England. It is located 1 kilometre (0.6 mi) south of Glossop Town Hall, south of Glossop Brook between Bray Clough and Hurst Brook. The urban area stretches about 1 kilometre (0.6 mi) up the hillside. Whitfield was one of the original townships in the ancient parish of Glossop, and in the manor. The ancient township rose from 150 to 544 metres above mean sea level, and the upper part is part of the Peak District National Park. The highest point is Mill Hill which is on the Pennine Way.
Swineshaw Reservoir is a 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 by the Duke of Norfolk. Swineshaw, on Swineshaw Clough, was adopted in 1864 by the Glossop Water Company to provide drinking water for Glossop. It was taken over in 1929 by the Glossop Corporation Waterworks. This became part of the Manchester Corporation Waterworks in 1959. Swineshaw, Hurst Reservoir and Mossy Lea Reservoir are no longer in service.
Hurst Reservoir was 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 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.
The Mottram Tunnel is a tunnel carrying drinking water by gravity from Arnfield Reservoir, Tintwistle, Derbyshire, in the valley of the River Etherow, to Godley, Greater Manchester, in the valley of the River Tame. It was essential to the construction of the Longdendale Chain of reservoirs constructed by John Frederick Bateman. The tunnel was built between August 1848 and October 1850, and the Godley service reservoir was built to receive and filter the water. That was finished in 1851.
The Birmingham Corporation Water Department was responsible for the supply of water to Birmingham, England, from 1876 to 1974. It was also known as Birmingham Corporation Waterworks Department.
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.