- River Chess
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Coordinates: 51°42′22″N 0°36′36″W / 51.706°N 0.610°W
Contents
The River Chess is a chalk stream which springs from Chesham, Buckinghamshire and runs through Buckinghamshire and Hertfordshire, in south-eastern England. The Chess, along with the Colne and Gade, gives rise to the name of the district of Three Rivers, in which it forms its confluence with the Colne. The River Chess falls 60 m and is 17.9 km long.
Etymology
Its name arose by back-formation from the name of Chesham.
River flow
The river rises from springs in the Vale of Chesham and in Pednor before flowing in a south-easterly direction past Waterside. The river banks are mostly not public rights of way, and only small stretches of the river are accessible. Beyond Latimer it flows to the north of Chenies and on towards Rickmansworth after which it becomes a tributary of the River Colne. It is navigable only in its lower reaches.
Drought
The river suffered from a severe lack of water for approximately two years between 2004 and 2006. The cause of this was believed to be a lack of rainfall.
Wildlife
The Chess Valley is one of the most attractive parts of the Chilterns Area of Natural Beauty (AONB), with a rich natural and cultural history. It supports several key species listed in the Government's UK Biodiversity Action Plan, including water vole, water rail, kingfisher, stream water crowfoot and brown trout. There is a head of coarse fish; however, this is not in abundance.
Human influences
The valley has a long history of human habitation. There are a number of Roman villa sites along the valley, including Latimer Park. At Sarratt strip lynchets can be seen in terraces along the hillside made by the action of ploughing along the slope and thought to have been the site of medieval vineyards.
Human habitation has altered the valley and the river in many ways, not all of them beneficial for wildlife. River modifications such as dredging and widening slow the current, allow silt to accumulate and smother the gravel riverbed. Changes in the land use adjacent to the river can also have impact. Water meadows have been replaced by arable fields and building developments, altering drainage patterns and causing pollution. Abstraction of water from the underlying chalk aquifer reduces river flows and lowers the river's ability to tolerate drought.
The introduction of alien species to the catchment has had a major effect on the wildlife of the river. Water vole populations declined catastrophically along the Chess between 2001 & 2003 with a 97% population decrease being observed. This population crash was caused mainly by the North American mink, a species introduced to the British Isles originally for the fur trade. In 2004 a water vole recovery project was set up by the Chilterns Chalk Streams Project, BBOWT and the Environment Agency, combining mink control with habitat improvement to try to halt this decline. In 2005 a survey found that the water vole population had recovered to 18% of its 2001 levels.
A less positive story is that of the native white-clawed crayfish, which has suffered at the hands of another American import, the signal crayfish. Originally imported by the aquaculture industry, the signal crayfish was seen as a way for trout farms to diversify and exploit new markets. However, due to their expert, escapologist nature, signal crayfish soon escaped into surrounding river systems and quickly spread throughout the majority of the UK's southern river system. Signal crayfish have carried crayfish plague, to which they are resistant, but which the native white-clawed crayfish has no defence against. The result has been the gradual eradication of native crayfish from the UK's rivers. In the case of the Chess, white-clawed crayfish have been extinct since the mid 1990s.
Not all imports have quite such a catastrophic effect. Another escapee into the Chess from fish farms and trout fisheries is the rainbow trout, thought to have been introduced to the Chess in the early 20th century. They have since gone on establish one of a handful of self-sustaining populations in the UK.
The Chess is also home to a number of invasive alien plant species including Japanese knotweed, Himalayan Balsam and orange balsam.
Chess cress
Historically the fertile land around the Chess was ideal for growing watercress and this industry flourished in both Chesham and Rickmansworth in the Victorian era. There are watercress beds at Church End, Sarratt. Today the Chess is equally well known for trout fishing.
Chess Valley Walk
The Chess Valley Walk is approximately 10 miles (16 km) long and links with the Metropolitan line stations of Chesham, Chorleywood and Rickmansworth giving visitors the chance to walk either part or the entire route. The route can be followed in either direction and is clearly waymarked. Most of the route is on public footpaths but there are short sections on roads. A walk leaflet can be downloaded free here: [1]
External links
- Chilterns Area of Outstanding Natural Beauty
- Watercress beds at Sarratt
- Chess Valley Archaeological and Historical Society
- Dry river bed in 2006
Rivers and Watercourses of Buckinghamshire Rivers and Watercourses of Hertfordshire Ash • Bayford Brook • Beane • Bulbourne • Chess • Colne • Cuffley Brook • Gade • Hiz • Ivel • Lea • River Lee Flood Relief Channel • Lee Navigation • Mimram • New River • Pix Brook • Quin • Rib • Stort • Stort Navigation • Small River Lea • VerCategories:- Chesham
- Geography of Three Rivers (district)
- Thames drainage basin
- Rivers of Buckinghamshire
- Rivers of Hertfordshire
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