Lee Valley Reservoir Chain

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Aerial view of several of the Lee Valley reservoirs Lee Valley Reservoirs.jpg
Aerial view of several of the Lee Valley reservoirs

The Lee Valley Reservoir Chain is located in the Lee Valley, and comprises 13 reservoirs that supply drinking water to London. [1]

Contents

The Reservoir Chain is a major geographic constraint; together with the Thames it is one of the two significant topographic features that divide the capital and define the communities on either side. The Lower Lea Valley, downstream of the reservoirs, is more integrated, with better east–west transport connectivity.

Geographic significance

The southern reservoirs, viewed from the north Aerial view of Walthamstow Reservoirs from the north.jpg
The southern reservoirs, viewed from the north

The Chain separates the London Boroughs of Haringey and Enfield to the west, from Waltham Forest and Essex in the east. The corridor includes 13 reservoirs, two to three channels of the Lee, as well as marshes and parkland, up to a mile wide.

During WWI, the settlements on both sides of the Lea were badly hit by Germany Army and Navy airship raids. It is believed the crews mistook the Reservoir Chain for the Thames and released their bombs on what they took to be central London. [2]

The Boundary Commission treats the Thames and Lea as natural barriers within London. When reviewing the boundaries of London's parliamentary constituencies, it concludes that any constituency spanning either river would be artificial and not reflect local communities or identities. The 2018 review compromised on this, allowing a cross-Lea constituency further south, in the Lower Lea where the communities on each side are more integrated due to greater quantity and quality of the road and rail links across the valley. [3]

The corridor is part of the Metropolitan Green Belt and its national and international significance for wildlife is reflected by SSSI, Ramsar and SPA designations. [4] Lying between some of Londons's most densely populated areas, the Reservoir Chain and associated open land provides a highly valued ecological, landscape and recreational resource for the people of north and east London.

Reservoirs

Aerial View of Walthamstow Reservoirs Aerial View of Walthamstow Reservoirs.jpg
Aerial View of Walthamstow Reservoirs

The following waters are located in the London Borough of Enfield and are known collectively as the Chingford Reservoirs, which are a Site of Special Scientific Interest: [5]

The following waters, together known as the Walthamstow Reservoirs, are located in the London Borough of Waltham Forest and, with the exception of one, form a Site of Special Scientific Interest: [5] [6]

The reservoirs have the following characteristics: [1]

Lee valley reservoirs
ReservoirWater Source (see below)Water SupplyDepth, metresCapacity, Ml
King George VRiver Lea, New River, Lea DiversionPumped7.512,500
William GirlingLea DiversionPumped12.516,500
BanburyLea Diversion & Thames-Lee tunnelPumped8.52,950
LockwoodLea Diversion & Thames-Lee tunnelPumped10.42,500
High MaynardLee Diversion, Walthamstow No. 4, East WarwickGravity-fed5.8680
Low MaynardHigh MaynardGravity-fed3.0150
East WarwickHigh Maynard, West WarwickGravity-fed5.8960
West WarwickEast WarwickGravity-fed5.8800
Walthamstow No. 4High Maynard, Walthamstow No. 5Gravity-fed5.8590
Walthamstow No. 5Walthamstow No. 4Gravity-fed5.8770

Water supply

The reservoirs are fed by the following waters:

Water treatment

After being stored in the above reservoirs the water is piped to the Coppermills Water Treatment Works to be treated. [8] In 2006 a smaller water treatment works was also built at Chingford at the edge of the William Girling and King George V reservoirs. [9]

See also

Related Research Articles

Chingford Human settlement in England

Chingford is a town in east London, England, within the ceremonial county of Greater London and the historic county of Essex. The ancient woodland, Epping Forest forms a border to the north and east, the Lea Valley reservoirs to the West and the A406 North Circular Road to the south. Chingford is situated 8.6 miles (13.8 km) north-east of Charing Cross, with Waltham Abbey to the north, Woodford Green and Buckhurst Hill to the east, Walthamstow to the south, and Edmonton and Enfield to the west. The town contains the areas of Chingford Green, Chingford Hatch, Chingford Mount, Friday Hill, Hale End, Highams Park, and South Chingford, and had a population of 66,211 at the 2011 census.

<span class="mw-page-title-main">Walthamstow</span> Town in East London

Walthamstow is a large town in North East London, England, within the ceremonial county of Greater London and the ancient county of Essex. Situated 7+12 miles northeast of Charing Cross, the town borders Chingford to the north, Snaresbrook and South Woodford to the east, Leyton and Leytonstone to the south, and Tottenham to the west. At the 2011 census, the town had a population of approximately 109,424.

<span class="mw-page-title-main">London Borough of Waltham Forest</span> London borough in United Kingdom

The London Borough of Waltham Forest is a London borough in north-east London, England. Its population is estimated to be 276,983 in 2019. It borders five other London boroughs: Enfield to the north-west, Haringey to the west, Hackney to the south-west, Newham to the south-east and Redbridge to the east, as well as the non-metropolitan county of Essex to the north.

<span class="mw-page-title-main">River Lea</span> River in the south east of England

The River Lea is in South East England. It originates in Bedfordshire, in the Chiltern Hills, and flows southeast through Hertfordshire, along the Essex border and into Greater London, to meet the River Thames at Bow Creek. It is one of the largest rivers in London and the easternmost major tributary of the Thames.

Sewardstone is a hamlet in the civil parish of Waltham Abbey, in the Epping Forest District of Essex, England. It is 11.6 miles north-northeast of Central London and is in the London commuter belt. In 2018 it had an estimated population of 1128.

<span class="mw-page-title-main">Walthamstow Marshes</span>

Walthamstow Marshes, is a 36.7 hectare biological Site of Special Scientific Interest in Walthamstow in the London Borough of Waltham Forest. It was once an area of lammas land – common land used for growing crops and grazing cattle.

The Lea Valley, the valley of the River Lea, has been used as a transport corridor, a source of sand and gravel, an industrial area, a water supply for London, and a recreational area. The London 2012 Summer Olympics were based in Stratford, in the Lower Lea Valley. It is important for London's water supply, as the source of the water transported by the New River aqueduct, but also as the location for the Lee Valley Reservoir Chain, stretching from Enfield through Tottenham and Walthamstow.

<span class="mw-page-title-main">William Girling Reservoir</span> Body of water

The William Girling Reservoir is located in the London Borough of Enfield and is part of the Lee Valley Reservoir Chain that supplies London with drinking water. It is named after William Girling OBE, a chairman of the Metropolitan Water Board (MWB). The reservoir and the nearby King George V Reservoir are known collectively as the Chingford Reservoirs. The storage reservoir, which is owned by Thames Water, is bordered by Chingford to the east and Ponders End and Edmonton to the west, and covers 334 acres with a perimeter of 3.5 miles (5.6 km). There is no public access.

<span class="mw-page-title-main">King George V Reservoir</span> Body of water

The King George V Reservoir, also known as King George's Reservoir, is located in the London Borough of Enfield and is part of the Lee Valley Reservoir Chain that supplies London with drinking water. The storage reservoir is bordered by Sewardstone and Chingford to the east and Brimsdown and Ponders End to the west, and covers 420 acres, making it the largest in London. The reservoir and the nearby William Girling Reservoir are known collectively as the Chingford Reservoirs, and are owned and managed by Thames Water.

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.

Lea Valley Walk Long-distance footpath in South East England

The Lea Valley Walk is a 50-mile (80 km) long-distance path located between Leagrave, the source of the River Lea near Luton, and the Thames, at Limehouse Basin, Limehouse, east London. From its source much of the walk is rural. At Hertford the path follows the towpath of the River Lee Navigation, and it becomes increasingly urbanised as it approaches London. The walk was opened in 1993 and is waymarked throughout using a swan logo.

Lee Flood Relief Channel

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.

<span class="mw-page-title-main">Lockwood Reservoir</span> Water storage reservoir in East London

Lockwood Reservoir is located in Walthamstow in the London Borough of Waltham Forest. It is one of the ten Walthamstow Reservoirs, which are part of the Lee Valley Reservoir Chain. The reservoirs supply drinking water to London and are owned by Thames Water.

High Maynard Reservoir is located in Walthamstow in the London Borough of Waltham Forest. The storage reservoir is one of the Lee Valley Reservoir Chain and supplies drinking water to London.

<span class="mw-page-title-main">Low Maynard Reservoir</span> Body of water

Low Maynard Reservoir is located in Walthamstow in the London Borough of Waltham Forest. The storage reservoir is part of the Lee Valley Reservoir Chain and supplies drinking water to London.

<span class="mw-page-title-main">West Warwick Reservoir</span> Body of water

West Warwick Reservoir is located in the London Borough of Waltham Forest at Walthamstow. The storage reservoir is part of the Lee Valley Reservoir Chain, which supplies drinking water to London. It is owned by Thames Water.

Coppermill Stream Waterway in East London

The Coppermill Stream is a short waterway near Walthamstow in the Lea Valley. Originally a minor tributary of the River Lea, the approximately 2-mile (3.2 km) long stream is now used as an aqueduct to transport water from the reservoirs in the Lea Valley to Coppermills Water Treatment Works. The stream is part of a Site of Metropolitan Importance.

Hall Farm Curve

The Hall Farm Curve is a disused 500 m (1,600 ft) length of railway line in Walthamstow, east London, that connected Chingford station with Stratford station until the closure of the section of line in September 1968. The track was lifted in 1970.

<span class="mw-page-title-main">Walthamstow Wetlands</span> Urban nature reserve in Walthamstow, East London

Walthamstow Wetlands is a 211-hectare nature reserve in Walthamstow, east London, adjacent to the historic Essex-Middlesex border on the River Lea. It is focused on the Walthamstow Reservoirs, built by the East London Waterworks Company between 1853 and 1904 as part of the Lee Valley Reservoir Chain. The site is one of the largest urban wetland nature reserves in Europe and is particularly important for wildlife due to its position within the Lee Valley. It serves as a byway for migrating, wintering and breeding birds. Visitors can freely access the site's natural, industrial and social heritage in one of the capital's most densely populated urban areas.

Coppermills Water Treatment Works Water treatment works in east London

The Coppermills Water Treatment Works is a large water treatment works in the Lea Valley in east London. Completed in 1969 by the Metropolitan Water Board, it is now owned and operated by Thames Water. In 2009, Coppermills was connected to the Thames Water Ring Main via the Northern Extension Tunnel, enabling the facility to be a major supplier of water to the whole London area. It is capable of supplying a maximum of 680 million litres of water per day.

References

  1. 1 2 Curtis, R; Chamberlain, A; Clarke, B; Harris, R; Wakeford, P. Algae in raw water storage reservoirs: A case study into the effect on rapid gravity filtration (PDF) (Technical report). Archived from the original (PDF) on 2012-03-07. Retrieved 2007-11-09.
  2. Castle, Ian (2008). London 1914-17: the Zeppelin menace. Oxford, UK: Osprey Pub. ISBN   978-1-84603-245-5. OCLC   166380089.
  3. 2018 Boundary Commission proposals for parliamentary constituencies https://boundarycommissionforengland.independent.gov.uk/wp-content/uploads/2018/09/Final-recommendations-report.pdf
  4. Walthamstow Wetlands SSSI details includes reference to other designations https://designatedsites.naturalengland.org.uk/SiteGeneralDetail.aspx?SiteCode=UK9012111&SiteName=&countyCode=&responsiblePerson=&unitId=&SeaArea=&IFCAArea=
  5. 1 2 "Lee Valley Regional Park Authority, Reservoirs". Archived from the original on 2010-03-09. Retrieved 2011-09-05.
  6. Natural England, Nature on the Map (Search on Walthamstow Reservoirs)
  7. Cuthbert, E W; Wood, F (Feb 1962). "The Thames-Lee Water Main". Proceedings of the Institution of Civil Engineers. 21 (2): 257–276. doi:10.1680/iicep.1962.05088. ISSN   1753-7789 . Retrieved 2022-07-30.
  8. "Coppermills" (PDF). Thames Water. Archived from the original (PDF) on 2007-10-20. Retrieved November 9, 2007.
  9. "Chingford South Water Treatment Works" (PDF). Retrieved 2022-08-18.

Coordinates: 51°35′N0°3′W / 51.583°N 0.050°W / 51.583; -0.050