Dovestone Reservoir

Yeoman Hey Reservoir is a reservoir in the English Peak District. On its margin is a commemorative stone laid by the King of Tonga in 1981. The reservoir is within the boundaries of Greater Manchester but was formerly in the West Riding of Yorkshire. It is one of three reservoirs in the same valley: above it is Greenfield Reservoir, and adjacent to and below it is Dovestone Reservoir. The reservoirs lie to the south of the A635 road across Saddleworth Moor. To the west, below the reservoirs, is the village of Greenfield.The reservoir scheme in the Greenfield Valley and Chew Valley by the Ashton Stalybridge and Dukinfield Waterworks Joint Committee commenced in 1870. Yeoman Hey was completed in 1880. Yeoman Hey and the valley's other reservoirs are owned by United Utilities.

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.

Greenfield Reservoir is a reservoir in the Saddleworth parish of the Metropolitan Borough of Oldham in Greater Manchester, in the English Peak District. Lying within the historic boundaries of the West Riding of Yorkshire, above the village of Greenfield, it is on the edge of the Peak District National Park, near the A635 road on Saddleworth Moor. The reservoir is fed by the Greenfield Brook and is above the Yeoman Hey Reservoir, which in turn feeds into Dovestone Reservoir. Ashton Stalybridge and Dukinfield Waterworks Joint Committee's reservoir scheme in the Greenfield Valley commenced in 1870. Greenfield and the valley's other reservoirs are owned by United Utilities.

Saddleworth Moor is a moorland in North West England. Reaching more than 1,312 feet (400 m) above sea level, it is in the Dark Peak area of the Peak District National Park. It is crossed by the A635 road and the Pennine Way passes to its eastern side.

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.

Chew Valley in Saddleworth, Greater Manchester, England, follows the course of Chew Brook on the western slopes of Black Chew Head to where it joins the River Tame at Greenfield, east of Manchester. Part of the higher fringes of the valley towards the peak of Black Chew Head lie across the boundary in Derbyshire. The eastern part of the valley including the reservoirs of Dovestone and Chew are within the north western extremity of the Peak District National Park. Chew Reservoir was completed in 1912. At 1,600 feet (490 m) above sea level, it was the highest reservoir constructed in England. A tram-road was laid in Chew Valley to transport 42,318 cubic yards (32,354 m3) of clay to make an inner core for its dam to make it watertight. The tram and railway are gone but the route forms the Oldham Way long-distance footpath; reconstructed bridge hosts a sign with information, pictures, and a map. In 1949, a BEA Douglas DC3 crashed into the hill at Wimberry Rocks killing 24 passengers and crew and leaving 8 survivors.

Uppermill Railway Station served the village of Uppermill in Oldham. It was built by the London and North Western Railway on their Micklehurst Line from Stalybridge to Diggle and Huddersfield. It opened in 1886 and closed to passengers in 1917. Regular passenger trains continued to pass through the station until 1964 and the line was closed completely in 1966.

The Huddersfield Narrow Canal is an inland waterway in northern England. It runs just under 20 miles (32 km) from Lock 1E at the rear of the University of Huddersfield campus, near Aspley Basin in Huddersfield, to the junction with the Ashton Canal at Whitelands Basin in Ashton-under-Lyne. It crosses the Pennines by means of 74 locks and the Standedge Tunnel.

Greenfield is a village in the civil parish of Saddleworth in the Metropolitan Borough of Oldham, in Greater Manchester, England. It is 4 miles (6.4 km) east of Oldham and 13 miles (21 km) north-east of Manchester. It is located in a broad rural area at the southern edge of the South Pennines; Dovestone Reservoir, Chew Reservoir and Greenfield Reservoir lie to the east of the village in the Peak District National Park.Historically part of the West Riding of Yorkshire, Greenfield is sited in the Chew Valley, on the main A635 road from Ashton-under-Lyne to Holmfirth.

Uppermill Civic Hall, also known as Saddleworth Civic Hall, is a municipal building in Lee Street, Uppermill, a village in Greater Manchester in England. The building currently serves as the offices and meeting place of Saddleworth Parish Council.

Uppermill is a village in the civil parish of Saddleworth in the Metropolitan Borough of Oldham, Greater Manchester, England. Historically in the West Riding of Yorkshire, it lies on the River Tame in a valley amongst the South Pennines with the Peak District National Park directly to the east, 5 miles (8.0 km) east of Oldham and 11 miles (17.7 km) northeast of Manchester. Uppermill and the neighbouring village of Dobcross have a combined population of 7,500.

Saddleworth Museum is an independent museum in Uppermill village, Saddleworth, Metropolitan Borough of Oldham, Greater Manchester, England. It is a registered charity and was accredited by the MLA. The museum opened in 1962 and is housed in the outbuildings of the Victoria Mill, a 19th-century mill building which stood beside the Huddersfield Narrow Canal. Its collections show the history of Saddleworth, which until 1974 local government reorganisation was part of the West Riding of Yorkshire. In September 2015 the museum closed for repair and remedial work to be undertaken and there was a temporary cabin in place while work on the building continued. the museum re-opened a year later in September 2016 after a £1.25 million refurbishment.