HOME
*



picture info

Kingsdale
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 Rowten Pot is one of several entrances into the lo ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

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 ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  




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 ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


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 ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


River Twiss
The River Twiss is a river in the county of Yorkshire, England. The source of the river is Kingsdale Beck which rises at Kingsdale Head at the confluence of Back Gill and Long Gill in the Yorkshire Dales. Beneath Keld Head, it changes its name to the River Twiss. It has two notable waterfalls, Thornton Force and Pecca Falls, and its course follows part of the Ingleton Waterfalls Walk, then through Swilla Glen to Thornton in Lonsdale and down to Ingleton, where it meets the River Doe to form the River Greta. The English landscape artist J. M. W. Turner was a frequent visitor to the area and his sketch of Thornton Force in 1816 is currently part of the Tate collection. Course From the caves below Keld Head there is a flow of water that joins Kingsdale Beck to form the River Twiss. It flows south over Thornton Force and Pecca Falls and through woodland to join the River Doe at Ingleton. Waterfalls The drop of Thornton Force is about . Pecca Falls has three drops totalling ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Yorkshire Dales
The Yorkshire Dales is an upland area of the Pennines in the Historic counties of England, historic county of Yorkshire, England, most of it in the Yorkshire Dales National Park created in 1954. The Dales comprise river valleys and the hills rising from the Vale of York westwards to the hilltops of the Pennine Drainage divide, watershed. In Ribblesdale, Dentdale and Garsdale, the area extends westwards across the watershed, but most of the valleys drain eastwards to the Vale of York, into the River Ouse, Yorkshire, Ouse and the Humber. The extensive limestone cave systems are a major area for caving in the UK and numerous walking trails run through the hills and dales. Etymology The word ''Dale (landform), dale'', like ''dell'', is derived from the Old English word ''dæl''. It has cognates in the North Germanic languages, Nordic/Germanic languages, Germanic words for valley (''dal'', ''tal''), and occurs in valley names across Yorkshire and Northern England. Usage here may have ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

Ingleton, North Yorkshire
Ingleton is a village and civil parish in the Craven district of North Yorkshire, England. The village is from Kendal and from Lancaster on the western side of the Pennines. It is from Settle. The River Doe and the River Twiss meet to form the source of the River Greta, a tributary of the River Lune. The village is on the A65 road and at the head of the A687. The B6255 takes the south bank of the River Doe to Ribblehead and Hawes. All that remains of the railway in the village is the landmark Ingleton Viaduct.OS map 98, Wensleydale and Upper Wharfdale. Arthur Conan Doyle was a regular visitor to the area and was married locally, as his mother lived at Masongill from 1882 to 1917 (see notable people). It has been claimed that there is evidence that the inspiration for the name Sherlock Holmes came from here. Whernside, north-north-east of the village, one of the Yorkshire Three Peaks, is the highest point in the parish at . There are major quarries within the paris ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


River Greta (Lune)
The River Greta is a river flowing through Lancashire and North Yorkshire in the north of England. The river is formed by the confluence of the River Twiss and the River Doe at Ingleton. From Ingleton, the Greta travels westwards through Burton-in-Lonsdale and, over the border in Lancashire, Cantsfield and Wrayton, passing Thurland Castle, where the Greta flows into the River Lune The River Lune (archaically sometimes Loyne) is a river in length in Cumbria and Lancashire, England. Etymology Several elucidations for the origin of the name ''Lune'' exist. Firstly, it may be that the name is Brittonic in genesis and der .... References Rivers of Lancashire Rivers of North Yorkshire Rivers of Lancaster 1Greta {{England-river-stub ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

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 ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

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 ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  




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 ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

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 ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]  


picture info

National Park
A national park is a nature park, natural park in use for conservation (ethic), conservation purposes, created and protected by national governments. Often it is a reserve of natural, semi-natural, or developed land that a sovereign state declares or owns. Although individual nations designate their own national parks differently, there is a common idea: the conservation of 'wild nature' for posterity and as a symbol of national pride. The United States established the first "public park or pleasuring-ground for the benefit and enjoyment of the people", Yellowstone National Park, in 1872. Although Yellowstone was not officially termed a "national park" in its establishing law, it was always termed such in practice and is widely held to be the first and oldest national park in the world. However, the Tobago Main Ridge Forest Reserve (in what is now Trinidad and Tobago; established in 1776), and the area surrounding Bogd Khan Mountain, Bogd Khan Uul Mountain (Mongolia, 1778), wh ...
[...More Info...]      
[...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]