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 The Upper Derwent Valley in the Peak District National Park

 Geology
 History
 When the Water Came
 The Upper Derwent Landscape Today
 Managing Tourism in the Upper Derwent Valley

 Problems in the Valley?

 Points to Consider

The Upper Derwent Valley in the Peak District National Park

Derwant valley montage Derwant valley montage Derwant valley montage

Map of the Upper Derwent Valley

The River Derwent rises high on the gritstone moors of Bleaklow and flows down the Derwent Valley to join the Woodlands Valley at Ladybower Reservoir.

It is a beautiful area, extremely popular with walkers, cyclists, fishermen and many day visitors. 


Geology

Derwent Reservoir
Derwent Reservoir

Gritstone creates the high moorland plateau on either side of the valley.  The rock was formed about 300 million years ago, when sands and muds were washed down from mountains to the north into a vast river delta. Pressure consolidated the sand and mud into gritstone and shale. Layers of both these rocks can be seen in the valley sides. Landslips have occurred where shale has become soft and overlying rocks have become unstable. Alport Castles is a famous example of such a landslip and is protected as a Site of Special Scientific Interest (SSSI).

Geology image

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History

Many hundreds of years ago, the Upper Derwent Valley area was used as a summer hunting ground for early hunter/gatherers. Little is known of the first settlers, who came later.

After the Norman Conquest in 1066, the Upper Derwent Valley became part of the Royal Forest of the Peak. This was a hunting reserve (not a forest in the modern sense) and there were harsh punishments for local people who cut peat, gathered wood or hunted animals in the Forest. An ancient bridleway ran through the valley from Derwent to Glossop and was used by the trains of packhorses transporting goods across the Peak District.

The Forest area was given to Welbeck Abbey in Nottinghamshire and then, in the 16th century, to William Cavendish (who became the Earl of Devonshire). Derwent Hall in the village of Derwent, was built in 1672 by the Belguy family. It was later owned by the Duke of Norfolk and became a Youth Hostel in 1931.

A turnpike road (where the owner charged a fee or toll for the use of the road) was built through the Woodlands Valley by Thomas Telford in 1819. This road was named the Snake Road in honour of the Duke of Devonshire, whose crest is a snake. The road passed through the village of Ashopton, which grew with the increased traffic. At the end of the 19th century Derwent and Ashopton were two typical Peak District villages. The land around was not very fertile but there were 14 farms scattered in and around the valley. although the population was small, the villages had churches, a school, inns and shops.

The village of Derwent before the valley was flooded
The village of Derwent before the valley was flooded

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When the Water Came

A reservoir is a man-made lake used to store water. It is usually formed by damming a deep narrow valley with a river running through.  Damming the valley allows the river water to be collected so flooding the valley.

The Upper Derwent Valley was very attractive for building reservoirs as it had long deep valleys with narrow points for dam building, a high rainfall (average 1350 mm per year) and an almost uninhabited moorland catchment area.

The Peak District is surrounded by a number of large industrial towns with a great demand for water. The Derwent Valley Water Board was set up in 1899 to supply water to Derby, Nottingham, Sheffield and Leicester. Gothic style dams were built to contain the waters of Howden Reservoir (1912) and Derwent Reservoir (1916). Birchinlee village was built to house the workers and their families. Although sites for further reservoirs were earmarked, at the time there was not enough demand.

Water image

It was later decided to build one very large reservoir, Ladybower. This flooded the part of the valley where the villages of Derwent and Ashopton lay. New houses were built for the villagers at Yorkshire Bridge. A viaduct was built to carry the Snake Road over the reservoir at Ashopton and another for the road to Yorkshire Bridge. The packhorse bridge at Derwent, which had a Preservation Order on it, was moved stone by stone and rebuilt at Slippery Stones at the head of the Howden Reservoir. The graves in the churchyard were excavated and the bodies reburied in an extension to Bamford churchyard.

Ladybower reservoir was completed in 1945.

With the dam complete, the waters gradually rose and the remains of the demolished villages disappeared. The Derwent church tower was left standing at first but that too was demolished in 1947.


Water Companies

A Water Act was passed in 1973 and in 1974 the Derwent Valley Water Board's reservoirs and land were transferred to the newly formed Severn Trent Water Authority, the second largest in the country. The Water Act of 1989 privatised the water industry and Severn Trent Water became a private company.

There were concerns that land of high conservation and recreation value might be sold by the water companies. However, provision in the Act states that the Countryside Commission must be consulted before the sale of land owned by the water company in a National Park.


Water Supply

Catchment area 19,850 hectares
Reservoir capacity 463692 million litres (3 reservoirs)
Treatment works Yorkshire Bridge, opened 1929
Water filtered, chlorine added and pH corrected Bamford Stage I opened 1948
Bamford Stage II opened 1967


Where the water goes: (millions of litres)

450 (untreated)

Sheffield
172 (treated)

77 Derbyshire

68 Leicester

27 Nottingham

 

In 1943 the Ladybower Dam was used for practice runs by the 617 Dambusters Squadron of Lancaster Bombers. These were in preparation for the assault on the very similar Ruhr Valley dams in Germany, which were bombed in May 1943.

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The Upper Derwent Valley Landscape Today

Moorland

After the last Ice Age - about 14,000 years ago - woodland spread over the Peak District. About 4 - 5,000 years ago, hunter/gatherers spread over the area, cutting and burning the trees to create clearings for hunting. This clearing of the land and the change in the climate, which was becoming cooler and wetter, produced peat bogs on flat areas (peat is the remains of sphagnum moss, preserved by acid, wet conditions).

A Grough
A grough

The vegetation of the peat bogs consists mainly of cotton grass. Groughs (gullies) and haggs (islands of peat left when most has eroded away) often have crowberry and bilberry growing on their edges where the peat is drier. On the better drained land heather, bilberry, cowberry, bracken, mat grass and purple moor grass for the vegetation.

Grouse, which are shot by parties of hunters between 12 August and 10 December, feed on the young heather and nest in the taller patches. The heather moors are managed for grouse by burning small patches in winter (to encourage new young shoots to grow). Much of the moorland has been declared a Site of Special Scientific Interest (SSSI) because of its special vegetation and rare birds, such as the golden plover. It has been proposed as a Special Protection Area for birds under a European Directive.

 

Farming

The farmers in this area are usually tenants. The typical hill farm has sheep and some cattle. There is enclosed (walled) land and some reclaimed moorland near to the farm and the farmer has grazing rights on the higher moorland. The sheep spend most of their lives on the moorland and high rough pastures. They are brought down for lambing, shearing and dipping. The white-faced woodland sheep is traditional in this area. The cattle are store cattle which are bred for beef but which are sold on to more fertile lowland farms at about six months old to be fattened.

Farming image

Woodland and Forest

The original woodlands of the valley have been reduced by cutting and grazing and are now confined to a few areas. Ladybower Clough is one such area. These woods are protected from grazing so that trees such as sessile oak, birch and rowan can regenerate from seed.

The Severn Trent Water Company owns 829 hectares of planted woodland and the Forestry Commission owns another 430 hectares. Most of these woodlands are conifers (larch, pine and spruce) with some broadleaved trees such as oak, beech and sycamore. As trees are cut for timber, young trees are planted. Conifers are not natural in the Peak District, but provide a habitat for some birds of prey and a few smaller birds.

 

Water

Woodland and Forest

As the reservoirs hold very acid water, they support little wildlife except for some wildfowl such as red-breasted mergansers. Trout are put into the reservoirs for anglers. Common sandpipers nest on the shores but are easily disturbed - leaflets now encourage anglers and picnickers to leave them in peace when they are rearing young. The streams often have grey wagtails and dippers.

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Managing Tourism in the Upper Derwent Valley

The Derwent valley has been popular since the opening of the turnpike roads and the development of coaching routes. The Peak District National Park Visitor Survey of 1986/87 found that around 1.25 million people visit the general area each year and on a summer Sunday there may be up to 4,000 people and 600 parked cars. Until 1981 there was little provision for visitors in the valley. The roads were often congested on busy weekends causing chaos and problems of access for local farmers, foresters and emergency services.

Car Park and picnic area at Fairholmes
Car park and picnic area at Fairholmes

A partnership Management Plan was written to try and solve some of these problems. Representatives were drawn from the Peak District National Park Authority, the Water Authority, Forestry Commission, National Trust, local councils and other interested parties. The joint action and funding of this management project has been a key point in its success. The scheme won awards for Tourism Enterprise (1982) and Conservation (1988).


Management Plan Achievements


Reducing problems of congestion through:

1. Traffic-free roads. Road north of Fairholmes are closed to motor traffic at peak times and to coaches all the time. A minibus is provided. The road east from Fairholmes is closed to non-local motor traffic.

2. Six new and improved car parks for 450 cars and 3 coaches have been provided, including one at Fairholmes (200 cars).

3. Bus services from surrounding towns and cities have been improved.

Cycle Hire
Cycle Hire

Valley Bus Service
Valley Bus Service

Improving wildlife conservation through:

1.  Carrying out a detailed ecological survey and implementing recommendations.

Conserving the distinctive character of the area through:

1. Landscape improvement schemes including the removal of concrete post and wire fencing.

2. A tree planting scheme increasing broadleaved plantations and improved the appearance of the landscape.

3. Opening up views across the reservoir.

Improving Facilities for Recreation through:

Visitor Centre at Fairholmes

Visitor Centre at Fairholmes

Ranger liasing with local Police

Ranger liasing with local Police

1. A new building at Fairholmes providing an enlarged Visitor Centre plus refreshments and toilets.  Publications on local history and walks are sold at the Visitor Centre and a free illustrated visitors' guide is available on request.

2. A cycle hire centre established in 1987. Around 15,000 cycles are now hired each year.

3. A full-time ranger, employed jointly by the National Park Authority and Severn Trent Water, appointed to carry out liaison with local farmers, landowners and visitors.

4. New and improved footpaths waymarked from the car park at Fairholmes, including a section for wheelchairs. 12 miles of new concessionary routes agreed.

5. Boat fishing allowed with a now well-established and popular trout fishery. A platform for disabled anglers at Ladybower. Sub aqua diving also takes place at Ladybower.

6. Attractive information boards interpreting popular features and sites.


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Problems in the Valley?

Providing recreation facilities is not always plain sailing ......


In 1981 proposals to allow sailing on Ladybower reservoir met stiff opposition. Ladybower Sailing Club (formed in 1980) made a planning application to the Peak District National Park Authority to build a sailing club on the northern arm of the reservoir. Opponents, including the National Trust, the Nature Conservancy Council (now English Nature) and the Ramblers Association argued that important species of ducks, and other birds could be driven away. A beautiful landscape could also be ruined. The application was refused.

An appeal was made in 1984 against the planning decision not to allow the sailing club on the northern arm of the reservoir. A further proposal for a base on the southern arm was put forward. Severn Trent Water opposed this as it was considered an unsafe site and would conflict with other recreational activities in the area. The appeal was dismissed and it was decided that no site for sailing could be found on the Ladybower reservoir.

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Points to Consider

What would your reaction have been if you had lived in the valley and been told it would be flooded and so you had to move?

What might the areas of conflict be today in the valley?  How could these be resolved?

For more information on any of the subjects highlighted in this factsheet try searching the archive.

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