Greenfield Reservoir

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.

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.

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.

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.

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.

Chew Reservoir is a reservoir at the head of the Chew Valley in the Peak District National Park in Greater Manchester, England. The reservoir scheme in the Greenfield and Chew Valleys by the Ashton Stalybridge and Dukinfield Waterworks Joint Committee commenced in 1870. Chew Reservoir was built to hold 200 million gallons of water. Intended to be a compensation reservoir, it also had a filtration plant so that it could be used for drinking water in times of drought. Completed in 1912, the reservoir was the highest constructed in England, at 1,600 feet (488 m) above sea level, until the Cow Green Reservoir in the North Pennines in Teesside was completed in 1971. The reservoir is connected to the larger Dovestone Reservoir further down the Chew Valley by the Chew Brook.

Standedge () is a moorland escarpment in the Pennine Hills of northern England between Marsden, West Yorkshire and Diggle, Greater Manchester. Standedge has been a major moorland crossing point since Roman times and possibly earlier. From east to west, Standedge is crossed by five generations of road crossing, the earliest a Roman road from York to Chester and the latest the A62 road. The Huddersfield Narrow Canal and the railway line from Leeds to Manchester pass underground in the Standedge Tunnels. The Pennine Way long-distance footpath passes through Standedge in a north–south direction along the Pennines. Much of Standedge is in the National Trust's Marsden Moor Estate. Administratively, Standedge is split between Kirklees and Oldham.

Diggle railway station was a station that served the village of Diggle on the Huddersfield Line to the north of Uppermill. Immediately to the west of the Standedge tunnels, it was opened in 1849 along with the first rail tunnel and closed to passenger traffic in 1968. In its heyday, the station had platforms serving all four lines but little trace remains of it today—all of the buildings and much of platforms having been demolished (although the nearby signal box remains operational). On 5 July 1923, an express passenger train, hauled by Ex-LNWR Whale Experiment Class 4-6-0 No. 1406 George Findlay, was in a rear-end collision with a freight train. Four people were killed.Local residents have periodically campaigned for the station to be reopened. This has often been connected to proposals to fully reopen the Standedge Tunnels.In 2012, a renewed effort was launched by a local Liberal Democrat parish councillor. This was unsuccessful, as Transport for Greater Manchester concluded that much of the cited passenger demand would actually be abstracted from the existing station at nearby Greenfield.

The Standedge Tunnels () are four parallel tunnels through the Pennine hills at the Standedge crossing between Marsden in Kirklees, West Yorkshire and Diggle in Oldham, Greater Manchester in northern England. Three are railway tunnels (containing the Huddersfield line) and the other is a canal tunnel. Before boundary changes in 1974, both ends of the tunnels were in the West Riding of Yorkshire. The canal tunnel on the Huddersfield Narrow Canal was authorised by an Act of Parliament on 4 April 1794. Construction of a 5,451-yard (4,984 m) tunnel began months later. Within two years, cost-saving measures pushed back its completion date and progress was slowed by water levels much greater than had been expected. It proved difficult to secure skilled help, some tenders went unanswered and Benjamin Outram withdrew from the venture. In 1807, Thomas Telford drew up a new plan for its completion. In 1811, the tunnel opened. It is the longest and oldest of the four Standedge tunnels and is the longest, highest, and deepest canal tunnel in the United Kingdom. Having been closed to all traffic in 1943, the canal tunnel was re-opened in May 2001. The first, single-track railway tunnel, built for the London and North Western Railway (LNWR) on its line between Huddersfield and Manchester, was completed in 1848. It proved to have insufficient capacity and a second, parallel, single-track tunnel was opened in 1871. The LNWR opened a third, double-track tunnel in 1894. Only the double-track tunnel is currently used for rail traffic; the other two are intact but disused. All four tunnels are linked by cross-tunnels or adits at strategic intervals which allowed the railway tunnels to be built without construction shafts and allowed waste material to be removed by boat. The Standedge Tunnel Visitor Centre, at the Marsden end, is a base for boat trips into the tunnel and has an exhibition depicting the different crossings.

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.

Diggle is a village in the civil parish of the Saddleworth in Metropolitan Borough of Oldham, in Greater Manchester, England. The village is situated on the moorlands of the Pennine hills. Historically part of the West Riding of Yorkshire, it is located at one end of the restored Standedge Canal Tunnel, Britain's longest, deepest and highest canal tunnel. In the village there is a listed building, the Gate pub and a post office/off-licence. Diggle is home to Diggle F.C., an FA registered amateur football club which plays its home games at Churchill Playing Fields, Uppermill. It competes in the Huddersfield and District Association Football League. Saddleworth Clarion Cycling Club host the annual Beard Cup Hill Climb out of Diggle each September.

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.