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Dentdale
Dentdale is a dale or valley in the north-west of the Yorkshire Dales National Park in Cumbria, England. It is the valley of the River Dee, but takes its name from the village of Dent. The dale runs east to west, starting at Dent Head, which is the location of a railway viaduct on the Settle-Carlisle Line. Dentdale is one of the few Yorkshire Dales that drain westwards to the Irish Sea. History Dentdale was first settled in the 10th century when Norse invaders first entered the dale. The dale was also known to the Romans although there is no evidence of settlement during that period. The dale was one of the last of the Yorkshire Dales to be Enclosed in 1859. The typical occupations in the dale were farming and worsted related. Several mills used the fast flowing waters of the River Dee to supply power to the mills. At least one of these was converted to the Dent Marble industry by 1810. Whilst fishing on the Dee at Dentdale in the 1840s, William Armstrong saw a waterwh ...
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Dentdale - Geograph
Dentdale is a dale or valley in the north-west of the Yorkshire Dales National Park in Cumbria, England. It is the valley of the River Dee, but takes its name from the village of Dent. The dale runs east to west, starting at Dent Head, which is the location of a railway viaduct on the Settle-Carlisle Line. Dentdale is one of the few Yorkshire Dales that drain westwards to the Irish Sea. History Dentdale was first settled in the 10th century when Norse invaders first entered the dale. The dale was also known to the Romans although there is no evidence of settlement during that period. The dale was one of the last of the Yorkshire Dales to be Enclosed in 1859. The typical occupations in the dale were farming and worsted related. Several mills used the fast flowing waters of the River Dee to supply power to the mills. At least one of these was converted to the Dent Marble industry by 1810. Whilst fishing on the Dee at Dentdale in the 1840s, William Armstrong saw a waterwh ...
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Dent, South Lakeland
Dent is a village and civil parishes in England, civil parish in Cumbria, England, within the historic boundaries of the West Riding of Yorkshire. It lies in Dentdale, a narrow valley on the western slopes of the Pennines within the Yorkshire Dales National Park, south east of Sedbergh and north east of Kirkby Lonsdale. At the United Kingdom Census 2011, 2011 census, Dent and Middleton, Cumbria, Middleton had a total population of 785. History Historically, Dent was part of the Ewecross wapentake in the West Riding of Yorkshire. From 1894 to 1974 it was part of Sedbergh Rural District. In 1974 it became part of the new county of Cumbria. The origin of the name is debated. Older forms include ''Denet'' (1200). It may have been taken from the hill now known as Dent Crag (2,250 ft), to be compared with another hill named Dent near Cleator in Cumberland, in which case it would derive from a pre-English Celtic languages, Celtic term related to Old Irish ''dinn, dind'' "a hil ...
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Dales Way
The Dales Way is an long-distance footpath in Northern England, from (south-east to north-west) Ilkley, West Yorkshire, to Bowness-on-Windermere, Cumbria. This walk was initially devised by the West Riding Ramblers' Association with the 'leading lights' being Colin Speakman and Tom Wilcock (Footpath Secretary). The route was announced to the public in 1968 and the first recorded crossing was by a group of Bradford Grammar School Venture Scouts in 1969. The Dales Way passes through two National Parks: the Yorkshire Dales National Park and the Lake District National Park. The first half of the walk follows the River Wharfe upstream to the main watershed of Northern England at Ribblehead. The second half follows several river valleys (Dentdale, River Mint, River Kent) to descend to the shores of Windermere. Route The walk is shorter and less strenuous than better-known routes such as the Pennine Way and Coast to Coast Walk, being mostly along river valleys. It thus makes a go ...
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River Dee, Cumbria
The River Dee is a river running through the extreme south east of Cumbria, a part of the Craven region traditionally part of the West Riding of Yorkshire. Its name possibly derives from Brythonic ''deva'' meaning ''goddess'', or from Dent or Dentdale, through which the river flows. The river rises above Dent Head Farm (on the Dales Way), formed from several smaller streams emanating from Blea Moor Moss, the River Dee makes its way northward past Stone House, where it is joined by Arten Gill, to Cowgill, where it turns left into Dentdale. In Dentdale, it picks up the waters of Deepdale Beck (travelling north from Whernside) before passing Dent and Gawthrop. The river later passes Lenacre and Rash on its way to meeting the River Rawthey at Catholes, near the town of Sedbergh. The old water mill at Rash Bridge is thought to have been an inspiration for the folk song "The Jolly Miller of Dee". The Rawthey goes on to join the River Lune The River Lune (archaically sometime ...
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River Dee (Lune)
The River Dee is a river running through the extreme south east of Cumbria, a part of the Craven region traditionally part of the West Riding of Yorkshire. Its name possibly derives from Brythonic ''deva'' meaning ''goddess'', or from Dent or Dentdale, through which the river flows. The river rises above Dent Head Farm (on the Dales Way), formed from several smaller streams emanating from Blea Moor Moss, the River Dee makes its way northward past Stone House, where it is joined by Arten Gill, to Cowgill, where it turns left into Dentdale. In Dentdale, it picks up the waters of Deepdale Beck (travelling north from Whernside) before passing Dent and Gawthrop. The river later passes Lenacre and Rash on its way to meeting the River Rawthey at Catholes, near the town of Sedbergh. The old water mill at Rash Bridge is thought to have been an inspiration for the folk song "The Jolly Miller of Dee". The Rawthey goes on to join the River Lune The River Lune (archaically sometimes ...
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Dent Head Viaduct
Dent Head Viaduct is a railway viaduct on the Settle–Carlisle line in Dentdale, Cumbria, England. It is the second major viaduct on the line northwards after Ribblehead Viaduct, and is just north of Blea Moor Tunnel at milepost 251, and to the south of Arten Gill Viaduct. Construction of the viaduct began in 1869, and it was completed in 1875, extra time being needed due to periods of heavy rainfall. The line bows slightly to the east in order to follow the contours of Woldfell, which it navigates on the western side. The viaduct was grade II Listed in 1999. Dent Head Viaduct is north of Settle Junction, and south of railway station. History The viaduct is long, high, and consists of ten arches which are each across. The parapets of the viaduct are measured at above sea level. The spans are grouped into two sets of five, separated by a larger pier in the middle. The viaduct is constructed from a local limestone known as ''Blue Limestone'', which was quarried from Short G ...
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Arten Gill Viaduct
Arten Gill Viaduct is an eleven-arch railway bridge in Dentdale, Cumbria, England. The viaduct carries the Settle to Carlisle railway line over Artengill Beck. The viaduct was originally designed to be further west, which is lower down the steep valley side, but by moving the line slightly eastwards, the viaduct could be installed at a higher location, thereby using fewer materials in its height. Arten Gill Viaduct is constructed partly from Dent Marble in the inside of the arches instead of the more usual brick. Dent Marble is a type of dark limestone which was quarried from Artengill beneath the viaduct itself. The viaduct is a grade II listed structure, and a scheduled monument. History Groundwork on site was started in May 1870, with work on the viaduct itself beginning a year later, on 3 May 1871. The parapets were completed in July 1875, with the date being set into the middle stone on each side of the parapet wall. Arten Gill Viaduct is long, and high, with the parapets ...
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Gawthrop
Gawthrop is a hamlet in the South Lakeland district, in the county of Cumbria, England. Historically part of the West Riding of Yorkshire, it lies within the Yorkshire Dales National Park. It is near the River Dee and the village of Dent Dent may refer to: People * Dent (surname) * Dent May (active 2007), American musician * Dent Mowrey (1888–1960), American composer, musician and music teacher * Dent Oliver (1918–1973), international speedway rider Places France * Dent d' .... See also * Listed buildings in Dent, Cumbria References Hamlets in Cumbria Dent, Cumbria {{Cumbria-geo-stub ...
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William Armstrong, 1st Baron Armstrong
William George Armstrong, 1st Baron Armstrong, (26 November 1810 – 27 December 1900) was an English engineer and industrialist who founded the Armstrong Whitworth manufacturing concern on Tyneside. He was also an eminent scientist, inventor and philanthropist. In collaboration with the architect Richard Norman Shaw, he built Cragside in Northumberland, the first house in the world to be lit by hydroelectricity. He is regarded as the inventor of modern artillery. Armstrong was knighted in 1859 after giving his gun patents to the government. In 1887, in Queen Victoria's golden jubilee year, he was raised to the peerage as Baron Armstrong of Cragside. Early life Armstrong was born in Newcastle upon Tyne at 9 Pleasant Row, Shieldfield, about a mile from the city centre. Although the house in which he was born no longer exists, an inscribed granite tablet marks the site where it stood. At that time the area, next to thPandon Dene was rural. His father, also called William, wa ...
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Dent Fault
The Dent Fault is a major fault zone on the boundary between the counties of Cumbria and North Yorkshire in northern England. It is named after the village of Dent in Dentdale, on the western margin of the Yorkshire Dales. The fault, or rather the 'Dent Fault System' – a collection of closely associated faults and folds, defines the western edge of the Askrigg Block, a geological structure that underlies the Yorkshire Dales. The fault is associated with the Taythes Anticline to its west and the Fell End Syncline to its east. Other than vertical movement on the fault, there has also been an element of strike-slip movement. To the north, the fault links with the Pennine Fault System in the vicinity of Brough and with the Craven Fault System near Kirkby Lonsdale to the south.Stone et al. 2010 ''British Regional Geology: Northern England'' (5th edition) Keyworth, Notts, British Geological Survey Regional setting The Carboniferous geology of northern England consists of a series ...
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Yorkshire Dales National Park
The Yorkshire Dales National Park is a national park in England covering most of the Yorkshire Dales. Most of the park is in North Yorkshire, with a sizeable area in Westmorland (Cumbria) and a small part in Lancashire. The park was designated in 1954, and extended in 2016. Over 95% of the land in the Park is under private ownership; there are over 1,000 farms in this area. In late 2020, the park was named as an International Dark Sky Reserve. This honour confirms that the area has "low levels of light pollution with good conditions for astronomy". Some 23,500 residents live in the park (as of 2017); a 2018 report estimated that the Park attracted over four million visitors per year. The economy consists primarily of tourism and agriculture. Location The park is north-east of Manchester; Otley, Ilkley, Leeds and Bradford lie to the south, while Kendal is to the west, Darlington to the north-east and Harrogate to the south-east. The national park does not include all of ...
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Inclosure Acts
The Inclosure Acts, which use an archaic spelling of the word now usually spelt "enclosure", cover enclosure of open fields and common land in England and Wales, creating legal property rights to land previously held in common. Between 1604 and 1914, over 5,200 individual enclosure acts were passed, affecting 28,000 km2. History Before the enclosures in England, a portion of the land was categorized as "common" or "waste". "Common" land was under the control of the lord of the manor, but certain rights on the land such as pasture, pannage, or estovers were held variously by certain nearby properties, or (occasionally) ''in gross'' by all manorial tenants. "Waste" was land without value as a farm strip – often very narrow areas (typically less than a yard wide) in awkward locations (such as cliff edges, or inconveniently shaped manorial borders), but also bare rock, and so forth. "Waste" was not officially used by anyone, and so was often farmed by landless peasants. The ...
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