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Fountains Fell Tarn
Fountains Fell Tarn, is an upland lake between the two peaks of Fountains Fell, in North Yorkshire, England. The tarn is close to the Pennine Way, some north west of Malham Tarn, and east of Horton in Ribblesdale. Water from the tarn flows eastwards through Cowside Beck, which is a tributary of the River Skirfare in Littondale. Whilst the water in the lake is acidic, as it runs off the mountain, it flows over Yoredale beds limestone and so becomes a harder (more alkaline) water. Description Fountains Fell Tarn occupies a shallow basin created by glacial activity in the Devensian age, which scoured the limestone away. Malham Tarn was created in a similar fashion with the removal of the porous limestone allowing water to collect. Although the tarn does not have a permanent outflow (the inflow of water almost matching that of the evaporation), in times of heavy precipitation, water from the tarn drains eastwards as Cowside Beck, an affluent of the River Skirfare in Littond ...
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Fountains Fell
A fountain, from the Latin "fons" (genitive "fontis"), meaning source or spring, is a decorative reservoir used for discharging water. It is also a structure that jets water into the air for a decorative or dramatic effect. Fountains were originally purely functional, connected to springs or aqueducts and used to provide drinking water and water for bathing and washing to the residents of cities, towns and villages. Until the late 19th century most fountains operated by gravity, and needed a source of water higher than the fountain, such as a reservoir or aqueduct, to make the water flow or jet into the air. In addition to providing drinking water, fountains were used for decoration and to celebrate their builders. Roman fountains were decorated with bronze or stone masks of animals or heroes. In the Middle Ages, Moorish and Muslim garden designers used fountains to create miniature versions of the gardens of paradise. King Louis XIV of France used fountains in the Gardens of ...
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River Wharfe
The River Wharfe ( ) is a river in Yorkshire, England originating within the Yorkshire Dales National Park. For much of its middle course it is the county boundary between West Yorkshire and North Yorkshire. Its valley is known as Wharfedale. The watercourse first becomes known as the River Wharfe at the confluence of Greenfield Beck and Oughtershaw Beck at Beckermonds. Flowing initially through Langstrothdale, it then passes by, or in some cases through, Kettlewell, Grassington, Bolton Abbey, Addingham, Ilkley, Burley-in-Wharfedale, Otley, Wetherby and Tadcaster. It then flows into the River Ouse near Cawood. The section of the river from its source to around Addingham is in Upper Wharfedale and has a very different character to the river downstream. The Wharfe is long (before it joins the Ouse), making it the 21st longest river in Britain. It is a public navigation from the weir at Tadcaster to its junction with the Ouse near Cawood and is tidal from Ulleskelf to the Ouse ...
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List Of Lakes And Tarns In North Yorkshire
This is a list of lakes and tarns in North Yorkshire, England. Unlike the nearby Lake District, North Yorkshire does not have many natural lakes due to the porosity of the limestone underneath the surface. The JNCC Special Area of Conservation status for the Craven Limestone Complex lists running and standing Water at only 1%. Upland tarns are common where the underlying stone allows the water to collect. These tarns are usually surrounded by peat, so most have relatively acidic water in comparison to the alkaline nature of water which runs over Limestone common in the area. Man-made reservoirs and dams, such as at Moss Dam in Swaledale, are not included, as the list focuses only on natural lakes and tarns. The list only covers those within Yorkshire, and sites such as Sunbiggin Tarn, whilst in the Yorkshire Dales National Park, are not included, as that body of water is in the county of Cumbria. Some tarns or lakes may no longer exist; historical documents refer to Gigglesw ...
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Halton Gill
Halton Gill is a hamlet and civil parish in Littondale in the Yorkshire Dales in North Yorkshire, England. It is situated up Littondale from Litton. A minor road leads south west to Silverdale and Stainforth in Ribblesdale. The name of the hamlet was recorded in 1457 as Haltonghyll. The name derives from a combination of Old English and Old Norse and means the nook of land (or ravine) with a small valley by a farmstead and a stream. The civil parish includes the hamlets of Foxup and Hesleden. To the south the parish rises to the summits of Plover Hill and Pen-y-Ghent. The population of the civil parish was estimated at 60 in 2012. From Halton Gill there is a bridleway over the Horse Head Pass to the north east to Yockenthwaite in Langstrothdale. This path was used by the priest from Hubberholme to reach the small chapel in Halton Gill. To the west paths lead to the summit of Pen-y-ghent via Plover Hill. The 2010 Sainsbury's Christmas advert with celebrity chef, Jamie O ...
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Pen-y-ghent
Pen-y-ghent or Penyghent is a fell in the Yorkshire Dales, England. It is the lowest of Yorkshire's Three Peaks at ; the other two being Ingleborough and Whernside. It lies east of Horton in Ribblesdale. It has a number of interesting geological features, such as Hunt Pot, and further down, Hull Pot. The waters that flow in have created an extensive cave system which rises at Brants Gill head. In 2004 the body of Lamduan Armitage, dubbed by the media the "Lady of the Hills", was found near to the entrance of Sell Gill Hole. Etymology In the Cumbric language, exactly as in today's Welsh, ''pen'' meant 'top' or 'head', and ''y'' is most likely the definite article (''the''), exactly as in Modern Welsh ''y'' (compare Pen-y-berth 'end of the hedge/copse', or Pen-y-ffordd 'head of the road/way', etc.). The element ''ghent'' is more obscure, it could be taken to be 'edge' or 'border'. The name ''Pen-y-ghent'' could therefore mean 'Hill on the border' (compare Kent). Or else, the fi ...
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Silverdale, North Yorkshire
Silverdale is a minor Dale (landform), dale in the Yorkshire Dales in North Yorkshire, England. It is a side dale of Ribblesdale, and lies west of Fountains Fell. The dale head is just south of Pen-y-ghent. The Pennine Way crosses the head of the dale. A minor road runs through the dale from Stainforth, North Yorkshire, Stainforth to Halton Gill. along the road from Stainforth is the site of Neolithic burial ground known as Giants Graves. References External links

{{coord, 54, 08, 11.7, N, 2, 14, 37.3, W, display=title, region:GB_type:dale Yorkshire Dales Valleys of North Yorkshire ...
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Old Norse
Old Norse, Old Nordic, or Old Scandinavian, is a stage of development of North Germanic languages, North Germanic dialects before their final divergence into separate Nordic languages. Old Norse was spoken by inhabitants of Scandinavia and their Viking expansion, overseas settlements and chronologically coincides with the Viking Age, the Christianization of Scandinavia and the consolidation of Scandinavian kingdoms from about the 7th to the 15th centuries. The Proto-Norse language developed into Old Norse by the 8th century, and Old Norse began to develop into the modern North Germanic languages in the mid-to-late 14th century, ending the language phase known as Old Norse. These dates, however, are not absolute, since written Old Norse is found well into the 15th century. Old Norse was divided into three dialects: Old West Norse, ''Old West Norse'' or ''Old West Nordic'' (often referred to as ''Old Norse''), Old East Norse, ''Old East Norse'' or ''Old East Nordic'', and ''Ol ...
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Fountains Abbey
Fountains Abbey is one of the largest and best preserved ruined Cistercian monasteries in England. It is located approximately south-west of Ripon in North Yorkshire, near to the village of Aldfield. Founded in 1132, the abbey operated for 407 years, becoming one of the wealthiest monasteries in England until its dissolution, by order of Henry VIII, in 1539. In 1983, Studley Royal Park including the ruins of Fountains Abbey was purchased by the National Trust. The abbey is maintained by English Heritage. Foundation After a dispute and riot in 1132 at the Benedictine house of St Mary's Abbey in York, 13 monks were expelled, among them Saint Robert of Newminster. They were taken under the protection of Thurstan, Archbishop of York, who provided them with land in the valley of the River Skell, a tributary of the Ure. The enclosed valley had all the natural features needed for the creation of a monastery, providing shelter from the weather, stone and timber for building, and ...
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Hard Water
Hard water is water that has high mineral content (in contrast with "soft water"). Hard water is formed when water percolates through deposits of limestone, chalk or gypsum, which are largely made up of calcium and magnesium carbonates, bicarbonates and sulfates. Hard drinking water may have moderate health benefits. It can pose critical problems in industrial settings, where water hardness is monitored to avoid costly breakdowns in boilers, cooling towers, and other equipment that handles water. In domestic settings, hard water is often indicated by a lack of foam formation when soap is agitated in water, and by the formation of limescale in kettles and water heaters.World Health OrganizatioHardness in Drinking-Water 2003 Wherever water hardness is a concern, water softening is commonly used to reduce hard water's adverse effects. Origins Natural rainwater, snow and other forms of precipitation typically have low concentrations of multivalent cations such as calcium and magnes ...
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River Aire
The River Aire is a major river in Yorkshire, England, in length. The ''Handbook for Leeds and Airedale'' (1890) notes that the distance from Malham to Howden is direct, but the river's meanderings extend that to . Between Malham Tarn and Airmyn, the river drops . Part of the river below Leeds is canalised, and is known as the Aire and Calder Navigation. Course The Aire starts at Malham Tarn and becomes a subterranean stream at 'Water Sinks' about one mile (1.6 km) before the top of Malham Cove, it then flows underground to Aire Head, just below Malham, in North Yorkshire, and then flows through Gargrave and Skipton. After Cononley, the river enters West Yorkshire where it passes through the former industrial areas of Keighley, Bingley, Saltaire and Shipley. It then passes through Leeds and on to Swillington and Woodlesford. At Castleford is the confluence of the Aire and Calder; just downstream of the confluence was the ford where the ancient British road, used by t ...
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North Yorkshire
North Yorkshire is the largest ceremonial counties of England, ceremonial county (lieutenancy area) in England, covering an area of . Around 40% of the county is covered by National parks of the United Kingdom, national parks, including most of the Yorkshire Dales and the North York Moors. It is one of four counties in England to hold the name Yorkshire; the three other counties are the East Riding of Yorkshire, South Yorkshire and West Yorkshire. North Yorkshire may also refer to a non-metropolitan county, which covers most of the ceremonial county's area () and population (a mid-2016 estimate by the Office for National Statistics, ONS of 602,300), and is administered by North Yorkshire County Council. The non-metropolitan county does not include four areas of the ceremonial county: the City of York, Middlesbrough, Redcar and Cleveland and the southern part of the Borough of Stockton-on-Tees, which are all administered by Unitary authorities of England, unitary authorities. ...
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