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Dovestone Reservoir

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Dovestones from Alphin Hill
Dovestones from Alphin Hill

Dove Stone Reservoir lies at the convergence of the valleys of the Greenfield and Chew Brooks above the village of Greenfield, on Saddleworth Moor in Greater Manchester, England. The reservoir is on the western edge of the Peak District National Park. It supplies drinking water to the surrounding area and is a tourist attraction, providing several walks amongst picturesque landscapes.

Excerpt from the Wikipedia article Dovestone Reservoir (License: CC BY-SA 3.0, Authors, Images).

Dovestone Reservoir
Chew Road,

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Latitude Longitude
N 53.53 ° E -1.975 °
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Dovestone Sailing Club

Chew Road
OL3 7NE , Saddleworth
England, United Kingdom
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dovestonesc.org.uk

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Dovestones from Alphin Hill
Dovestones from Alphin Hill
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Greenfield Valley
Greenfield Valley

Greenfield Valley is a river valley through Saddleworth Moor in England's Peak District National Park. Historically this area of the South Pennines was part of Yorkshire but since 1974 it has been within the eastern edge of the county of Greater Manchester.The valley and the surrounding Saddleworth Moor are designated as 'Open Access' land for the public, following the Countryside and Rights of Way Act 2000. Much of Saddleworth Moor is a 9,000 year-old peat landscape of blanket bog. The upper Greenfield Valley is part of the Dark Peak SSSI (Site of Special Scientific Interest). The millstone grit moorland is typically covered with grasses, mosses, heather and bilberry and is habitat for mountain hares and moorland birds such as red grouse, lapwing, skylark, curlew, golden plover and meadow pipit. The RSPB operates Dove Stone Nature Reserve in the valley, which includes old quarry cliffs that are home to peregrine falcons.The Trinnacle is a dramatic large stack of three gritstone pillars at Raven Stones Brow. Since glaciers and ice sheets carved the cliff edge during the last Ice Age, weathering and frost-shattering of the rocks over thousands of years have formed the three-pronged Trinnacle outcrop. There are nearly 200 graded rock climbing routes on Ravenstones Crag.The valley's main stream Greenfield Brook is fed by Holme Clough and Birchen Clough. Greenfield Brook flows into Greenfield Reservoir and then on into Yeoman Hey Reservoir and Dovestone Reservoir. It then flows into Chew Brook which is a tributary of the River Tame, which feeds the River Mersey.The Ashton under Lyne, Stalybridge and Dukinfield Waterworks Joint Committee's reservoir scheme began in the Greenfield Valley in 1870. Yeoman Hey Reservoir was completed in 1880 (capacity of 780 million litres and 20m deep). Greenfield Reservoir was built from 1897 to 1902. It is the smallest of the reservoirs (capacity of 464 million litres and 20m deep). Dovestone Reservoir is the largest of the three reservoirs in the valley. It has a capacity of 4887 million litres and is up to 31m deep. The dam is 38m high and 550m long. It was built in 1967 and the Dovestone Sailing Club was established the same year. The reservoirs are operated by United Utilities and supply water to the surrounding area including Oldham. Spruce and pine plantations are found in the lower valley and broad-leaved trees have been introduced to provide a more diverse habitat. Industrialist John Platt built Ashway Gap House in 1850 on the south side of the valley. It was used as a shooting lodge until his brother James (MP for Oldham) was killed in a grouse shooting accident on the moors in 1857. Ashway Cross was erected on the moorland as a memorial to James. The vacant mansion and its estate were bought in 1897 by the waterworks board, which allowed it to be used as a Red Cross hospital for wounded soldiers during World War I. In World War II the house was used to billet Italian prisoners of war. After the house fell into decline it was demolished in 1981.There are two World War II pillboxes (gun emplacements) on the A635 road opposite Yeoman Hey Reservoir. The pillboxes were built into a rock outcrop in c.1940 as part of defences against a possible invasion. The pair are connected by an underground passage. They are protected Grade II listed buildings.Downstream from the reservoirs is Greenfield village in the Chew Valley.

Saddleworth
Saddleworth

Saddleworth is a civil parish of the Metropolitan Borough of Oldham in Greater Manchester, England. It comprises several villages and hamlets as well as suburbs of Oldham on the west side of the Pennine hills. Areas include Austerlands, Delph, Denshaw, Diggle, Dobcross, Friezland, Grasscroft, Greenfield, Grotton, Lydgate, Scouthead, Springhead and Uppermill.Saddleworth lies east of Oldham and 11 miles (17.7 km) northeast of Manchester. It is broadly rural and had a population of 25,460 at the 2011 Census, making it one of the larger civil parishes in the United Kingdom. Historically in the West Riding of Yorkshire and following the Industrial Revolution, in the 18th and 19th centuries, Saddleworth became a centre for cotton spinning and weaving. By the end of Queen Victoria's reign, mechanised textile production had become a vital part of the local economy. The Royal George Mill, owned by the Whitehead family, manufactured felt used for pianofortes, billiard tables and flags. Following the Great Depression Saddleworth's textile sector declined. Much of Saddleworth's architecture and infrastructure dates from its textile processing days however, notably the Saddleworth Viaduct and several cottages and terraces, many built by the local mill owners. For centuries Saddleworth was linked, ecclesiastically, with the parish of Rochdale and was long talked of as the part of Yorkshire where Lancastrians lived. The former Saddleworth Urban District was the only part of the West Riding to have been amalgamated into Greater Manchester in 1974. However, strong cultural links with Yorkshire remain amongst its communities. There are several brass bands in the parish.