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Kingsdale Game Farm
Kingsdale is a valley on the western edge of the Yorkshire Dales National Park in northern England. The name Kingsdale derives from a combination of Old Norse and Old English (''Kyen'' and ''Dael'') which means ''The valley where the cows were kept''. Humans were active in Kingsdale from 6,700 BC onwards. Evidence of fire-pits used by hunter-gatherers have been found in the dale. The larger part of the valley lies within the county of North Yorkshire but its highest reaches fall just within Cumbria. It is defined by the hills of Whernside to its east and Gragareth to its west. Kingsdale is drained by the south-westward flowing Kingsdale Beck which assumes the name River Twiss before joining the River Doe at Ingleton to become the River Greta. The single minor public road which serves the valley is followed by the Yorkshire Dales Cycle Way. There are several nationally important caves within the valley (such as Rowten Pot and Yordas Cave) and the impressive resurgence of Keld ...
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Kingsdale Head - Geograph
Kingsdale is a valley on the western edge of the Yorkshire Dales National Park in northern England. The name Kingsdale derives from a combination of Old Norse and Old English (''Kyen'' and ''Dael'') which means ''The valley where the cows were kept''. Humans were active in Kingsdale from 6,700 BC onwards. Evidence of fire-pits used by hunter-gatherers have been found in the dale. The larger part of the valley lies within the county of North Yorkshire but its highest reaches fall just within Cumbria. It is defined by the hills of Whernside to its east and Gragareth to its west. Kingsdale is drained by the south-westward flowing Kingsdale Beck which assumes the name River Twiss before joining the River Doe at Ingleton, North Yorkshire, Ingleton to become the River Greta (Lune), River Greta. The single minor public road which serves the valley is followed by the Yorkshire Dales Cycle Way. There are several nationally important caves within the valley (such as Rowten Pot and Yordas ...
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River Doe
The River Doe is a river in North Yorkshire, England. The river's source is near God's Bridge close to the settlement of Chapel-le-Dale and flows through Twisleton in a south-westerly direction to Ingleton, where it meets the River Twiss to form the River Greta. The river forms part of the River Lune system that flows into the Irish Sea. Course The source of the river is found at a place named God's Bridge where Chapel Beck disappears underground and the Doe begins. The river flows south west, fed by a number of small unnamed springs on the valley sides. The first named tributary is Light Water Spring which feeds north west into the river near a disused quarry. Near Twisleton Dale House, the river can be crossed by some stepping stones at a fording point as well as some later near the disused granite quarry. Further down stream near Twisleton Hall there are another set of stepping stones at a fording point just above Beezley Falls. After flowing under a footbridge, there ar ...
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Valleys Of North Yorkshire
A valley is an elongated low area often running between hills or mountains, which will typically contain a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacial ice. These glaciers may remain present in valleys in high mountains or polar areas. At lower latitudes and altitudes, these glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry a watercourse only rarely. In areas of limestone bedrock, dry valleys may also result from drainage now taking place underground rather than at the surface. Rift valleys arise principally from earth movements, rather than erosion. Many different types of valleys are described by geographers, using terms that may be global in use or else applied only locally. For ...
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Craven District
Craven is a local government district of North Yorkshire, England centred on the market town of Skipton. In 1974, Craven District was formed as the merger of Skipton urban district, Settle Rural District and most of Skipton Rural District, all in the West Riding of Yorkshire. The population of the Local Authority area at the 2011 Census was 55,409. It comprises the upper reaches of Airedale, Wharfedale, Ribblesdale, and includes most of the Aire Gap and Craven Basin. The name Craven is much older than the modern district, and encompassed a larger area. This history is also reflected in the way the term is still commonly used, for example by the Church of England. History ''Craven'' has been the name of this district throughout recorded history. Note: Select the Thorton in Craven entry. Its extent in the 11th century can be deduced from The Domesday Book but its boundaries now differ according to whether considering administration, taxation or religion. Toponymy The deri ...
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Keld Head
Keld may refer to: * Keld, Cumbria, England *Keld, North Yorkshire, England *Variation of Kjell (name), a Danish given name * KELD (AM), a radio station (1400 AM) licensed to El Dorado, Arkansas, United States * KELD-FM KELD-FM (106.5 MHz) is a radio station licensed to Hampton, Arkansas Hampton is a town in Calhoun County, Arkansas, United States. The population was 1,324 at the 2010 census. The town is the county seat of Calhoun County. Hampton is part o ..., a radio station (106.5 FM) licensed to Hampton, Arkansas, United States * the ICAO code for South Arkansas Regional Airport at Goodwin Field {{disambiguation, geo, callsign, airport ...
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Spring (hydrosphere)
A spring is a point of exit at which groundwater from an aquifer flows out on top of Earth's crust (pedosphere) and becomes surface water. It is a component of the hydrosphere. Springs have long been important for humans as a source of fresh water, especially in arid regions which have relatively little annual rainfall. Springs are driven out onto the surface by various natural forces, such as gravity and hydrostatic pressure. Their yield varies widely from a volumetric flow rate of nearly zero to more than for the biggest springs. Formation Springs are formed when groundwater flows onto the surface. This typically happens when the groundwater table reaches above the surface level. Springs may also be formed as a result of karst topography, aquifers, or volcanic activity. Springs also have been observed on the ocean floor, spewing hot water directly into the ocean. Springs formed as a result of karst topography create karst springs, in which ground water travels throu ...
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Yordas Cave
Yordas Cave is a solutional cave in Kingsdale, North Yorkshire, England. It has been renowned since the eighteenth century as a natural curiosity, and was a show cave during the nineteenth century. It is now a popular destination for cavers, walkers, and outdoor activity groups. Description The old show cave entrance is in a plantation of trees from the road, at the base of a small cliff, at the bottom of a small gorge. A flight of three steps descend from the entrance archway into the Main Chamber, long, and wide. A stream flows across the floor, and disappears into some low passages to the left. Also on the left, a low passage can be followed for a few metres to the Back Door entrance in a shakehole. At the upstream end of the chamber two passages soon unite in the spray-lashed Chapter House chamber, where a waterfall enters and the showcave ended. Above the waterfall, a passage leads to a junction, with the water flowing from a low long passage which leads to the base o ...
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Rowten Pot
Rowten Pot is one of several entrances into the long cave system that drains Kingsdale in North Yorkshire, England. Its entrance is a shaft some long, wide, and at the southern end deep. Description A stream enters from just below the surface at the northern end. The cave is largely vertical, but at the bottom the stream flows through a short section of passage into the underground West Kingsdale river. This connects downstream with the ''Kingsdale Master Cave'' through three short sumps. Upstream, longer sumps may be followed up the valley for over , passing below the final pitch of Aquamole Pot. The cave is usually descended using single rope techniques, and is popular with cavers, being spacious and offering a variety of aerial routes. The three short sumps which connect to the Kingsdale Master Cave can be free-dived. The water which descends Rowten Pot sinks to the west of the pot on the other side of Turbary Road, into a shallow horizontal cave system, known as ''R ...
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Yorkshire Dales Cycle Way
Yorkshire ( ; abbreviated Yorks), formally known as the County of York, is a historic county in northern England and by far the largest in the United Kingdom. Because of its large area in comparison with other English counties, functions have been undertaken over time by its subdivisions, which have also been subject to periodic reform. Throughout these changes, Yorkshire has continued to be recognised as a geographic territory and cultural region. The name is familiar and well understood across the United Kingdom and is in common use in the media and the military, and also features in the titles of current areas of civil administration such as North Yorkshire, South Yorkshire, West Yorkshire and the East Riding of Yorkshire. Within the borders of the historic county of Yorkshire are large stretches of countryside, including the Yorkshire Dales, North York Moors and Peak District national parks. Yorkshire has been nicknamed "God's Own Country" or "God's Own County" by its i ...
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