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River Lea information


Lea
Lee
River Lea at Hertford Basin
Location
CountryUnited Kingdom
CountiesBedfordshire, Hertfordshire, Essex, Greater London
TownsLeagrave, Luton, Harpenden, Hatfield, Hertford, Ware, Hoddesdon, Broxbourne, Waltham Abbey, Enfield Town, Edmonton, Tottenham, Clapton, Stratford, Bow, Canning Town
Physical characteristics
Source 
 • locationLeagrave, Luton
 • coordinates51°54′37″N 0°27′40″W / 51.910338°N 0.461233°W / 51.910338; -0.461233
 • elevation115 m (377 ft)
Mouth 
 • location
Bow Creek, River Thames
 • coordinates
51°30′26″N 0°00′33″E / 51.5072°N 0.0092°E / 51.5072; 0.0092
 • elevation
0 m (0 ft)
Length68 km (42 mi)
Discharge 
 • locationLuton Hoo, Luton
 • average1.8 m3/s (64 cu ft/s)
Discharge 
 • locationFeildes Weir, Hoddesdon
 • average4.3 m3/s (150 cu ft/s)
Basin features
Designation
Ramsar Wetland
Official nameLea Valley
Designated9 October 2000
Reference no.1037[1]

The River Lea (/ˈl/ LEE) is in the East of England and Greater London. 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.

The river's significance as a major east–west barrier and boundary has tended to obscure its importance as north–south trade route. Below Hertford the river has since medieval times had alterations made to make it more navigable for boats between the Thames and eastern Hertfordshire and Essex, known as the Lee Navigation. This stimulated much industry along its banks. The navigable River Stort, the main tributary, joins it at Hoddesdon.

While the lower Lea remains somewhat polluted, its upper stretch and tributaries, classified as chalk streams, are a major source of drinking water for London. An artificial waterway known as the New River, opened in 1613, abstracts clean water away from the upper stretch of the river near Hertford for drinking, and lower parts of the river are also abstracted from. The Lea's origin in the Chilterns contributes to the extreme hardness (high mineral content) of London tap water.[2]

  1. ^ "Lee Valley". Ramsar Sites Information Service. Retrieved 25 April 2018.
  2. ^ "EC1A 7BE — Water quality in your area". Thames Water. Archived from the original on 27 May 2012. Retrieved 3 March 2012.

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