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Wessenden Valley
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 . 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 The Pennine Way is a National Trail in England, with a small section in Scotland. The trail stretches for from Edale, in the northern Derbyshire Peak District, north through the Yorkshire Dales and Northumberland National Park and ends at Kir ... 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 Marsden Moor Estate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Moorland
Moorland or moor is a type of habitat found in upland areas in temperate grasslands, savannas, and shrublands and montane grasslands and shrublands biomes, characterised by low-growing vegetation on acidic soils. Moorland, nowadays, generally means uncultivated hill land (such as Dartmoor in South West England), but also includes low-lying wetlands (such as Sedgemoor, also South West England). It is closely related to heath, although experts disagree on what precisely distinguishes these types of vegetation. Generally, moor refers to highland and high rainfall zones, whereas heath refers to lowland zones which are more likely to be the result of human activity. Moorland habitats mostly occur in tropical Africa, northern and western Europe, and neotropical South America. Most of the world's moorlands are diverse ecosystems. In the extensive moorlands of the tropics, biodiversity can be extremely high. Moorland also bears a relationship to tundra (where the subsoil is permafros ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dark Peak
The Dark Peak is the higher and wilder part of the Peak District in England, mostly forming the northern section but also extending south into its eastern and western margins. It is mainly in Derbyshire but parts are in Staffordshire, Cheshire, Greater Manchester, West Yorkshire and South Yorkshire. It gets its name because (in contrast to the White Peak), the underlying limestone is covered by a cap of Millstone Grit sandstones with softer shale underneath, meaning that in winter the soil is almost always saturated with water. The land is thus largely uninhabited moorland plateaux where almost any depression is filled with sphagnum bogs and black peat. The High Peak is an alternative name for the Dark Peak, but High Peak is also the name of an administrative district of Derbyshire which includes part of the White Peak. The areas of Millstone Grit form an 'inverted horseshoe' around the lower uncapped limestone areas of the White Peak, enclosing it to the west, north and east. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marsden, West Yorkshire
Marsden is a large village 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 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. History Marsden grew wealthy in the 19th century from the production of woollen cloth. It is still home to Bank Bottom Mill, later known as Marsden Mill, and home to John Edward Crowther Ltd, formerly one of the largest mills in Yorkshire. The Crowthers moved to Marsden in 1876, beginning a long and profitable association with cloth manufacturing in the town. During the 1930s Bank Bottom Mill covered an area of 14 acres, employed 680 looms, and provided employment for 1,900 workers. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
West Yorkshire
West Yorkshire is a metropolitan and ceremonial county in the Yorkshire and Humber Region of England. It is an inland and upland county having eastward-draining valleys while taking in the moors of the Pennines. West Yorkshire came into existence as a metropolitan county in 1974 after the reorganisation of the Local Government Act 1972 which saw it formed from a large part of the West Riding of Yorkshire. The county had a recorded population of 2.3 million in the 2011 Census making it the fourth-largest by population in England. The largest towns are Huddersfield, Castleford, Batley, Bingley, Pontefract, Halifax, Brighouse, Keighley, Pudsey, Morley and Dewsbury. The three cities of West Yorkshire are Bradford, Leeds and Wakefield. West Yorkshire consists of five metropolitan boroughs (City of Bradford, Calderdale, Kirklees, City of Leeds and City of Wakefield); it is bordered by the counties of Derbyshire to the south, Greater Manchester to the south-west, Lancash ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tributary
A tributary, or affluent, is a stream or river that flows into a larger stream or main stem (or parent) river or a lake. A tributary does not flow directly into a sea or ocean. Tributaries and the main stem river drain the surrounding drainage basin of its surface water and groundwater, leading the water out into an ocean. The Irtysh is a chief tributary of the Ob river and is also the longest tributary river in the world with a length of . The Madeira River is the largest tributary river by volume in the world with an average discharge of . A confluence, where two or more bodies of water meet, usually refers to the joining of tributaries. The opposite to a tributary is a distributary, a river or stream that branches off from and flows away from the main stream. PhysicalGeography.net, Michael Pidwirny & S ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Colne, West Yorkshire
The River Colne in West Yorkshire is formed at the confluence of two brooks that originate in the Pennines close to Marsden. It flows in an easterly direction through the Colne Valley and Huddersfield towards Cooper Bridge where it flows into the River Calder. Course Brooks formed by rainwater high (between 300 and 480 metres AMSL) in the Pennines of West Yorkshire, flow down the hillsides through the small valleys known locally as ''cloughs'' to fill March Haigh and Redbrook Reservoirs. The Haigh Brook and Redbrook continue down the valley fed by more tributaries, until they converge at a scenic spot called Close Gate Bridge where the River Colne is formed. The river flows from west to east through the Colne Valley passing through Marsden, Slaithwaite and Milnsbridge to Huddersfield and then on to Cooper Bridge where it feeds the larger River Calder. Its tributaries include Wessenden Brook, Bradley Brook, Crimble Brook, Mag Brook, Fenay Brook, New Mill Dike and the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Marsden Moor Estate
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wessenden Head Reservoir
Wessenden Head Reservoir is the highest in a series of four reservoirs in the Wessenden Valley above the village of Marsden in West Yorkshire, at the northern end of the Peak District National Park. Following the Wessenden Act of Parliament of 1836, Wessenden Reservoir was created by the construction of an earth embankment across Wessenden Brook. The Huddersfield Waterworks and Improvements Act of 1876 approved the building of a new reservoir above Wessenden Reservoir. Wessenden Head Reservoir was built between 1877 and 1881, fed from a catchwater drain via a sluice in the Shiny Brook (a tributary of Wessenden Brook). The Huddersfield Waterworks Act of 1890 led to Huddersfield Corporation purchasing the reservoirs from the Wessenden Commissioners in order to supply drinking water to the town. Wessenden Head Reservoir has a storage capacity of . The reservoir is currently owned and operated by Yorkshire Water. The Wessenden Valley Woodland Project was initiated in 2017 to develo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wessenden Reservoir
Wessenden Reservoir is the second in a series of four reservoirs in the Wessenden Valley above the village of Marsden in West Yorkshire, at the northern end of the Peak District National Park. Following the Wessenden Act of Parliament of 1836, the Wessenden Commissioners were established to build Wessenden Reservoir, to supply water to power the mills further down the valley and to protect people and property from floods. The reservoir was created by the construction of an earth embankment across Wessenden Brook. The reservoir ran dry during droughts in 1852, 1864 and 1865. The Huddersfield Waterworks Act of 1890 led to Huddersfield Corporation purchasing the reservoir from the Wessenden Commissioners in order to supply drinking water to the town. Wessenden Reservoir has a storage capacity of . The reservoir is currently owned and operated by Yorkshire Water. The Wessenden Valley Woodland Project was initiated in 2017 to develop natural habitats with increased biodiversity. T ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kirklees Way
The Kirklees Way is a 72-mile (115 km) waymarked footpath in Kirklees metropolitan district, West Yorkshire, England. It was opened in 1990 and includes the upper Colne Valley, Spen Valley and Holme Valley. The Peak District Boundary Walk The Peak District Boundary Walk is a circular walking trail, starting and finishing at Buxton and broadly following the boundary of the Peak District, Britain's first national park. The route was developed by the Friends of the Peak District (a ... follows the Kirklees Way for a few miles either side of Holme. References Further reading * External links Long Distance Walkers Association record for the Kirklees Way Tourist attractions in Kirklees Long-distance footpaths in England Protected areas of West Yorkshire Footpaths in West Yorkshire {{UK-trail-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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