Butterley Reservoir, West Yorkshire

The Wessenden Valley is a moorland valley in the Dark Peak, immediately south of Marsden in West Yorkshire, England. The name Wessenden derives from Old English and means the 'valley with rock suitable for whetstones'. The valley was formed by retreating glaciers at the end of the last ice age and continues to be cut by the Wessenden Brook a tributary of the River Colne with a catchment of 6.28 square miles (16.27 km2).The valley is in the Marsden Moor Estate and occupied by four reservoirs, namely Wessenden Head, Wessenden, Blakeley and Butterley, the largest. The Kirklees Way and Pennine Way long-distance footpaths follow the valley. The upper part of the valley near Wessenden Head is managed by the National Trust as part of the 5,000-acre (2,000 ha) Marsden Moor Estate.Butterley Reservoir's spillway, the only one of its kind in England, was a Grade II Listed structure until Yorkshire Water renovated it using concrete after winning a case on appeal.

Bank Bottom Mill, later known as Marsden Mill, was from 1824 an important centre for the production of woollen cloth in Marsden, West Yorkshire, England. Originally a fulling mill, Bank Bottom Mill reached its heyday in the late nineteenth and early twentieth centuries under the ownership of the Crowther family, in particular John Edward Crowther, a businessman and philanthropist. However, the cloth industry declined in the late twentieth century, and production of woollen cloth finally ceased in 2003.

Marsden is a large village in the Colne Valley, in the metropolitan borough of Kirklees, West Yorkshire, England. It is in the South Pennines close to the Peak District which lies to the south. The village is 7 miles (11 km) west of Huddersfield at the confluence of the River Colne and Wessenden Brook. It was an important centre for the production of woollen cloth. In 2020, the village had an estimated population of 3,768.

Marsden railway station serves the village of Marsden near Huddersfield in West Yorkshire, England. The station is on the Huddersfield Line, operated by Northern and is about 7 miles (11 km) west of Huddersfield station. It was opened in 1849 by the London & North Western Railway and is the last station before the West Yorkshire boundary with Greater Manchester. The station is operated by Northern Trains, but only Transpennine Express trains call here.

The Marsden Moor Estate is a large expanse of moorland in the South Pennines, between the conurbations of West Yorkshire and Greater Manchester in the north of England. It is named after the adjacent town of Marsden, and is owned and administered by the National Trust to whom it was conveyed in 1955 by the Radcliffe family in lieu of death duties. The estate covers 2,429 ha (5,685 acres) of unenclosed common moorland and almost surrounds Marsden. Part of it is in the most northern section of the Peak District National Park. The landscape is made up of moorland, valleys, peaks and crags and has long been modified by man. Marsden is at the eastern gateway to the important ancient Standedge crossing of the moors and evidence of transport related archaeological remains dating from pre-Roman times have been discovered close to the great engineering structures of the canal and railway ages. The moors have been a water catchment area since the Victorian era when several reservoirs were built, along with their associated catchwaters in the Wessenden Valley. The Pennine Way and the Peak District Boundary Walk run across the moors (following the same route between Wessenden and Redbrook Reservoirs.The landscape supports large numbers of moorland birds such as the golden plover, red grouse, Eurasian curlew and twite. The estate, a designated Site of Special Scientific Interest, forms part of a Special Protection Area and is a candidate Special Area of Conservation.The estate is managed from a base in the old goods yard, adjacent to Marsden railway station, and the old goods shed has been converted into a public exhibition, entitled Welcome to Marsden, which gives an overview of the estate and its history.The moor has been affected by fires. Dozens of firefighters were required to put out a blaze in 2011. A fire in February 2019, during an unseasonal spell of warm weather, was described by West Yorkshire Fire and Rescue Service as one of the biggest moorland fires it had ever had to deal with.

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.

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.

Deanhead Reservoir is a reservoir near Scammonden, in the metropolitan district of Kirklees, West Yorkshire, England. It is named after Dean Head, a village that was mostly submerged during construction of the dam. Construction started in 1838 and it opened a year later, almost 140 years before Scammonden Reservoir (its downstream neighbour) was opened in 1971. Water flowing out of Deanhead forms Black Burne Brook which now feeds into Scammonden Water. Deanhead reservoir was originally constructed to supply water to the factories in the Blackburn Valley that was downstream of the reservoir. During the 1995 drought, the outlines of foundations of buildings in the village were visible. Deanhead also is the name of a Pennine pass to the south of the reservoir, which carries the A640 from Huddersfield to Denshaw, following the course of a Roman road.

Wilberlee is a hamlet in the Colne Valley, in the Kirklees district, in the county of West Yorkshire, England. It is near the town of Huddersfield and the village of Slaithwaite. Wilberlee has a school called Wilberlee Junior and Infant School.

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.

Stott Hall Farm is a farm located between the eastbound and westbound carriageways of the M62 motorway in Calderdale, England. It is the only farm in the UK situated in the middle of a motorway and was built in the 18th century on Moss Moor. It lies south of Booth Wood Reservoir where the carriageways are separated between junctions 22 and 23. The road divides for much of its length between the Windy Hill and Deanhead cuttings because of the surrounding geography but a myth persists that it was split because the owners Ken and Beth Wild refused to sell.Sally Boazman, BBC Radio 2's traffic reporter and CB radio users nicknamed it the Little House on the Prairie. It is separated from the motorway by crash barriers and a fence to keep livestock in and prevent out-of-control vehicles crashing onto the property. It is one of the ten best-known sights on the motorway network. It was the subject of a BBC Radio 4 documentary, a Yorkshire Television documentary and a short film.