Marsden, West Yorkshire
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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.
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Kirklees
Kirklees is a local government district of West Yorkshire, England, governed by Kirklees Council with the status of a metropolitan borough. The largest town and administrative centre of Kirklees is Huddersfield, and the district also includes Batley, Birstall, West Yorkshire, Birstall, Cleckheaton, Denby Dale, Dewsbury, Heckmondwike, Holmfirth, Kirkburton, Marsden, West Yorkshire, Marsden, Meltham, Mirfield and Slaithwaite. Kirklees had a population of 422,500 in 2011; it is also the third largest metropolitan district in England by List of English districts by area, area size, behind Metropolitan Borough of Doncaster, Doncaster and City of Leeds, Leeds. History The borough was formed on 1 April 1974 by the provisions of the Local Government Act 1972 as part of a reform of local government in England. Eleven former local government districts were Amalgamation (politics), merged: the county boroughs of Huddersfield and Dewsbury, the municipal boroughs of Batley and Spenborough a ...
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Greater Manchester
Greater Manchester is a metropolitan county and combined authority, combined authority area in North West England, with a population of 2.8 million; comprising ten metropolitan boroughs: City of Manchester, Manchester, City of Salford, Salford, Metropolitan Borough of Bolton, Bolton, Metropolitan Borough of Bury, Bury, Metropolitan Borough of Oldham, Oldham, Metropolitan Borough of Rochdale, Rochdale, Metropolitan Borough of Stockport, Stockport, Tameside, Trafford and Metropolitan Borough of Wigan, Wigan. The county was created on 1 April 1974, as a result of the Local Government Act 1972, and designated a functional Manchester City Region, city region on 1 April 2011. Greater Manchester is formed of parts of the Historic counties of England, historic counties of Cheshire, Lancashire and the West Riding of Yorkshire. Greater Manchester spans , which roughly covers the territory of the Greater Manchester Built-up Area, the List of urban areas in the United Kingdom, second most ...
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Peel Street, Marsden, West Yorkshire
Peel or Peeling may refer to: Places Australia * Peel (Western Australia) * Peel Island, Queensland *Peel, New South Wales * Peel River (New South Wales) Canada * Peel Parish, New Brunswick * Peel, New Brunswick, an unincorporated community in Peel Parish * Peel River (Canada), tributary of the Mackenzie River * Peel Sound, Nunavut * Regional Municipality of Peel, Ontario (Peel County until 1973) :*Peel (federal electoral district) :*Peel (provincial electoral district) United Kingdom * Peel Fell, a hill in Kielder Forest * Peel Island, Cumbria * Peels, Northumberland, in Harbottle United States * Peel, Arkansas * Peel, Oregon Elsewhere * Peel, Isle of Man * Peel, Netherlands People Surname * Andrée Peel (1905–2010), member of the French Resistance during the Second World War * Ann Peel (born 1961), Canadian race walker * Arthur Peel (other) * Clifford Peel (1894–1918), Australian World War I pilot * Dwayne Peel (born 1981), Welsh rugby union player ...
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Standedge Tunnel End, Marsden, West Yorkshire
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. Surface crossings The earliest known crossing of Standedge is the Roman road connecting the Roman forts at Slack and Castleshaw, on the way from York to Chester. The road is believed to have been built in AD 80. Its course was ide ...
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List Of Geochronologic Names
This is a list of official and unofficial names for time spans in the geologic timescale and units of chronostratigraphy. Since many of the smallest subdivisions of the geologic timescale were in the past defined on regional lithostratigraphic units, there are many alternative names that overlap. The body concerned with standardizing the names of geochronologic units is the International Commission on Stratigraphy (ICS). In 2008 however, even though the Phanerozoic eon is almost completely divided into internationally recognizable units, local subdivisions are often still preferred over the international ones. List , , West, 1961 , - , Tiffanian , 60.2 , 56.8 , age , Paleocene , North America , , Granger, 1917 , - , Tiglian , 2.40 , 1.80 , super-age , Pleistocene , Netherlands , Tegelen (The Netherlands) , Dubois, 1905 , - , Tinguirirican , 36 , 29 , age , Oligo-Eocene , South America , , Flynn & Wyss, 2004 , - , Tithonian , 150.8 ± 4.0 , 145.5 ± 4.0 , age , Jurassic , ICS ...
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Carboniferous
The Carboniferous ( ) is a geologic period and system of the Paleozoic that spans 60 million years from the end of the Devonian Period million years ago ( Mya), to the beginning of the Permian Period, million years ago. The name ''Carboniferous'' means "coal-bearing", from the Latin '' carbō'' ("coal") and '' ferō'' ("bear, carry"), and refers to the many coal beds formed globally during that time. The first of the modern 'system' names, it was coined by geologists William Conybeare and William Phillips in 1822, based on a study of the British rock succession. The Carboniferous is often treated in North America as two geological periods, the earlier Mississippian and the later Pennsylvanian. Terrestrial animal life was well established by the Carboniferous Period. Tetrapods (four limbed vertebrates), which had originated from lobe-finned fish during the preceding Devonian, became pentadactylous in and diversified during the Carboniferous, including early amphibian line ...
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Stage (stratigraphy)
In chronostratigraphy, a stage is a succession of rock strata laid down in a single age on the geologic timescale, which usually represents millions of years of deposition. A given stage of rock and the corresponding age of time will by convention have the same name, and the same boundaries. Rock series are divided into stages, just as geological epochs are divided into ages. Stages can be divided into smaller stratigraphic units called chronozones. (See chart at right for full terminology hierarchy.) Stages may also be divided into substages or indeed grouped as superstages. The term faunal stage is sometimes used, referring to the fact that the same fauna (animals) are found throughout the layer (by definition). Definition Stages are primarily defined by a consistent set of fossils (biostratigraphy) or a consistent magnetic polarity (see paleomagnetism) in the rock. Usually one or more index fossils that are common, found worldwide, easily recognized, and limited to a sing ...
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Chronostratigraphy
Chronostratigraphy is the branch of stratigraphy that studies the ages of rock strata in relation to time. The ultimate aim of chronostratigraphy is to arrange the sequence of deposition and the time of deposition of all rocks within a geological region, and eventually, the entire geologic record of the Earth. The standard stratigraphic nomenclature is a chronostratigraphic system based on palaeontological intervals of time defined by recognised fossil assemblages (biostratigraphy). The aim of chronostratigraphy is to give a meaningful age date to these fossil assemblage intervals and interfaces. Methodology Chronostratigraphy relies heavily upon isotope geology and geochronology to derive hard dating of known and well defined rock units which contain the specific fossil assemblages defined by the stratigraphic system. In practice, as it is very difficult to isotopically date most fossils and sedimentary rocks directly, inferences must be made in order to arrive at an age d ...
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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 branch of the Campaign to Protect Rural England) and was launched on 17 June 2017. The Friends of the Peak District's founders, Gerald and Ethel Haythornthwaite, proposed the boundary of the Peak District National Park, which was subsequently established as the United Kingdom's first National Park in 1951. The route is waymarked with green markers and uses existing footpaths, tracks, quiet lanes, disused railway lines and a canal towpath. The start and finish is at the King's Head pub on Buxton Market Place, where a plaque has been installed by the Peak & Northern Footpaths Society (PNFS). The terrain covers open moorlands of the South Pennines, the limestone scenery of the Derbyshire Dales, woodlands, reservoirs and rural farming ...
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Spillway
A spillway is a structure used to provide the controlled release of water downstream from a dam or levee, typically into the riverbed of the dammed river itself. In the United Kingdom, they may be known as overflow channels. Spillways ensure that water does not damage parts of the structure not designed to convey water. Spillways can include floodgates and fuse plugs to regulate water flow and reservoir level. Such features enable a spillway to regulate downstream flow—by releasing water in a controlled manner before the reservoir is full, operators can prevent an unacceptably large release later. Other uses of the term "spillway" include bypasses of dams and outlets of channels used during high water, and outlet channels carved through natural dams such as moraines. Water normally flows over a spillway only during flood periods, when the reservoir has reached its capacity and water continues entering faster than it can be released. In contrast, an intake tower is a structure ...
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National Trust For Places Of Historic Interest Or Natural Beauty
The National Trust, formally the National Trust for Places of Historic Interest or Natural Beauty, is a charity and membership organisation for heritage conservation in England, Wales and Northern Ireland. In Scotland, there is a separate and independent National Trust for Scotland. The Trust was founded in 1895 by Octavia Hill, Sir Robert Hunter and Hardwicke Rawnsley to "promote the permanent preservation for the benefit of the Nation of lands and tenements (including buildings) of beauty or historic interest". It was given statutory powers, starting with the National Trust Act 1907. Historically, the Trust acquired land by gift and sometimes by public subscription and appeal, but after World War II the loss of country houses resulted in many such properties being acquired either by gift from the former owners or through the National Land Fund. Country houses and estates still make up a significant part of its holdings, but it is also known for its protection of wild lands ...
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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 ...
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