Community hub
Recent from talks
Contribute something to knowledge base
Content stats: 0 posts, 0 articles, 0 media, 0 notes
Members stats: 0 subscribers, 0 contributors, 0 moderators, 0 supporters
Subscribers
Supporters
Contributors
Moderators
Hub AI
Lea Valley AI simulator
(@Lea Valley_simulator)
Hub AI
Lea Valley AI simulator
(@Lea Valley_simulator)
Lea Valley
The Lea Valley (also spelt Lee 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.
The catchment area of the River Lea is located in the central part of the London Basin, on that basin's northern flank.
The main underlying geological formation of the upper part of the Lea catchment, north of Hoddesdon, is Cretaceous Chalk. The main underlying geological formation of the lower part of the Lea catchment, south of Hoddesdon, is Eocene London Clay.
However, large areas of these formations are overlain by much more recent Quaternary formations, including Clay-with-Flints (on the Chalk), till and other glacial deposits (mostly in the upper part of the catchment), and fluvial sand, gravel and alluvium (in the lower parts of today's valleys, but also on some higher ground in east Hertfordshire, Middlesex and west Essex, where such deposits were laid down by the pre-glacial "proto-Thames" and its former tributaries).
The northern boundary of the Lea catchment area rises to an altitude of almost 180 metres (590 ft), in hills north-east of Luton. The lowest point of the catchment area is the junction of the Lea with the Thames in east London, at an altitude of barely 5 metres (16 ft).
The relief of the upper part of the Lea catchment is one of gently rolling hills, which are divided by the valleys that fan out to the north and north-west from an area between Hertford and Hoddesdon.
The lower part of the Lea catchment runs from Hoddesdon southwards to east London, with the flood plain of the River Lea as its central feature. That flood plain has a width which extends to about 4.3 miles (7 km) in Edmonton. From there, the land rises on either side to an altitude of around 120 metres (390 ft), to gravel-capped plateaus in Hertfordshire (Northaw) and Middlesex (Southgate) to the west, and to Essex (Epping Forest) in the east.
The upper part of the catchment area of the River Lea was formerly a group of valleys whose rivers flowed approximately north–south directly into the River Thames (the "proto-Thames"). Until the Anglian glaciation about 450,000 years ago, the Thames flowed north-eastward past Watford, through what is now the Vale of St Albans, then eastwards towards Chelmsford and the North Sea.
Lea Valley
The Lea Valley (also spelt Lee 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.
The catchment area of the River Lea is located in the central part of the London Basin, on that basin's northern flank.
The main underlying geological formation of the upper part of the Lea catchment, north of Hoddesdon, is Cretaceous Chalk. The main underlying geological formation of the lower part of the Lea catchment, south of Hoddesdon, is Eocene London Clay.
However, large areas of these formations are overlain by much more recent Quaternary formations, including Clay-with-Flints (on the Chalk), till and other glacial deposits (mostly in the upper part of the catchment), and fluvial sand, gravel and alluvium (in the lower parts of today's valleys, but also on some higher ground in east Hertfordshire, Middlesex and west Essex, where such deposits were laid down by the pre-glacial "proto-Thames" and its former tributaries).
The northern boundary of the Lea catchment area rises to an altitude of almost 180 metres (590 ft), in hills north-east of Luton. The lowest point of the catchment area is the junction of the Lea with the Thames in east London, at an altitude of barely 5 metres (16 ft).
The relief of the upper part of the Lea catchment is one of gently rolling hills, which are divided by the valleys that fan out to the north and north-west from an area between Hertford and Hoddesdon.
The lower part of the Lea catchment runs from Hoddesdon southwards to east London, with the flood plain of the River Lea as its central feature. That flood plain has a width which extends to about 4.3 miles (7 km) in Edmonton. From there, the land rises on either side to an altitude of around 120 metres (390 ft), to gravel-capped plateaus in Hertfordshire (Northaw) and Middlesex (Southgate) to the west, and to Essex (Epping Forest) in the east.
The upper part of the catchment area of the River Lea was formerly a group of valleys whose rivers flowed approximately north–south directly into the River Thames (the "proto-Thames"). Until the Anglian glaciation about 450,000 years ago, the Thames flowed north-eastward past Watford, through what is now the Vale of St Albans, then eastwards towards Chelmsford and the North Sea.