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Wain Wath Force
Wain Wath Force is a waterfall on the River Swale in the Yorkshire Dales National Park, North Yorkshire, England. The falls are at grid reference , upstream from the hamlet of Keld which has three other waterfalls in its vicinity (Kisdon Force, East Gill Force, and Catrake Force). The names of waterfalls in the north of England often contain "force" after the Old Norse word ''foss'', which means "waterfall". Its name derives from the ford above the fall, ''wath'' being the Anglo-Saxon word for a ford. Wain may denote that it was passable for a cart or wain. Wain Wath Force is not a substantial waterfall: it has a drop of only around 1.5 metres as the river flows beneath the limestone cliffs of Cotterby Scar. Despite its modest height it is popular with visitors; the Coast to Coast long-distance footpath passes the falls on the north bank of the River Swale while the main motor road up Upper Swaledale Swaledale is one of the northernmost dales (valleys) in Yorkshire Dal ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wain Wath Force
Wain Wath Force is a waterfall on the River Swale in the Yorkshire Dales National Park, North Yorkshire, England. The falls are at grid reference , upstream from the hamlet of Keld which has three other waterfalls in its vicinity (Kisdon Force, East Gill Force, and Catrake Force). The names of waterfalls in the north of England often contain "force" after the Old Norse word ''foss'', which means "waterfall". Its name derives from the ford above the fall, ''wath'' being the Anglo-Saxon word for a ford. Wain may denote that it was passable for a cart or wain. Wain Wath Force is not a substantial waterfall: it has a drop of only around 1.5 metres as the river flows beneath the limestone cliffs of Cotterby Scar. Despite its modest height it is popular with visitors; the Coast to Coast long-distance footpath passes the falls on the north bank of the River Swale while the main motor road up Upper Swaledale Swaledale is one of the northernmost dales (valleys) in Yorkshire Dal ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Swale
The River Swale in Yorkshire, England, is a major tributary of the River Ure, which becomes the River Ouse, that empties into the North Sea via the Humber Estuary. The river gives its name to Swaledale, the valley through which it flows. The river and its valley are home to many types of flora and fauna typical to the Yorkshire Dales. Like similar rivers in the region, the river carves through several types of rock and has features typical of both river and glacial erosion. The River Swale has been a contributory factor in the settlements that have been recorded throughout its history. It has provided water to aid in the raising of crops and livestock, but also in the various mining activities that have occurred since Roman times and before. The river is said to be the fastest flowing in England and its levels have been known to rise in 20 minutes. Annual rainfall figures average 1800 mm p.a. in the headwaters and 1300 mm p.a. in the lower waters over a drop of 14 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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] |
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. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Keld, North Yorkshire
Keld is a village in the English county of North Yorkshire. It is in Swaledale, in the district of Richmondshire and the Yorkshire Dales National Park. The name derives from the Viking word ''Kelda'' meaning a spring and the village was once called ''Appletre Kelde'' – the spring near the apple trees. Keld is the crossing point of the Coast to Coast Walk and the Pennine Way long-distance footpaths at the head of Swaledale, and marks the end of the Swale Trail, a 20 km mountain bike trail which starts in Reeth. At the height of the lead-mining industry in Swaledale in the late 19th century, several notable buildings – now Grade II listed – were erected: they include the Congregational and Methodist chapels, the school and the Literary Institute. A tea room and small shop operate at Park Lodge from Easter to autumn. Out of season, local volunteers provide a self service café for visitors in the village’s Public Hall. Keld’s Youth Hostel closed in 2008 and has ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kisdon Force
Kisdon Force is a series of waterfalls on the River Swale in Swaledale, England. The falls are situated within the Yorkshire Dales National Park in the county of North Yorkshire, 500 metres downstream from the small hamlet of Keld at grid reference . Kisdon Force is one of several waterfalls on the Swale in the Keld area: the others are East Gill Force, Catrake Force and Wain Wath Force. All occur where the river cuts a gorge through the Carboniferous Limestone between the hills of Kisdon and Rogan's Seat. The falls in this area are termed "forces" after the Norse word ''fors'' or ''foss'', which means "waterfall". Both upper and lower Kisdon Force can be negotiated by canoeists, although a high degree of skill and experience is needed. The upper falls are rated Grade IV whilst the lower falls are rated more difficult at Grade V. The falls drop over two cascades and are surrounded by Kisdon Force Woods, a Site of Special Scientific Interest covering an area of 38 hectare ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
East Gill Force
East Gill Force is a waterfall in Swaledale, east of the hamlet of Keld, in the Yorkshire Dales National Park, North Yorkshire, England. The falls are located on East Gill at grid reference , just before its confluence with the River Swale at the point where the Pennine Way and the Coast to Coast Walk intersect. The falls are a popular spot for visitors, not just long-distance walkers but also families and picnickers because of the proximity of the road. East Gill Force has two main torrents: the upper falls have an impressive drop whilst the lower section is a series of stepped cascades that fall as East Gill enters the River Swale. East Gill Force is one of four waterfalls in the Keld area, the others being Kisdon Force, Catrake Force and Wain Wath Force that occur where the river cuts a gorge through the carboniferous limestone between the hills of Kisdon and Rogan's Seat Rogan's Seat is a remote hill located near East Stonesdale and Gunnerside Gill, in the Yorkshir ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Catrake Force
Catrake Force is a waterfall on the River Swale in North Yorkshire, England. It is not visible from the road but is accessible via a campsite in Keld. It comprises a series of four steps, each its own small waterfall, and each with a very different character – the largest single drop being about . It lies just upstream of Keld, downstream from Wain Wath Force. The next waterfall downstream is Kisdon Force. Waterfalls in the north of England are often termed ''Forces'' after the Norse word ''Foss'' which means waterfall, whilst Catrake derives from the Latin ''cataracta'' (waterfall) via Middle English. East Gill Force East Gill Force, a nearby waterfall on the tributary of East Gill just above its confluence with the Swale, is more obvious and accessible (being on both the Pennine Way and Coast to Coast Walk The Coast to Coast Walk is a long-distance footpath between the west and east coasts of Northern England, nominally long. Devised by Alfred Wainwright, it pa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Old English
Old English (, ), or Anglo-Saxon, is the earliest recorded form of the English language, spoken in England and southern and eastern Scotland in the early Middle Ages. It was brought to Great Britain by Anglo-Saxon settlement of Britain, Anglo-Saxon settlers in the mid-5th century, and the first Old English literature, Old English literary works date from the mid-7th century. After the Norman conquest of 1066, English was replaced, for a time, by Anglo-Norman language, Anglo-Norman (a langues d'oïl, relative of French) as the language of the upper classes. This is regarded as marking the end of the Old English era, since during this period the English language was heavily influenced by Anglo-Norman, developing into a phase known now as Middle English in England and Early Scots in Scotland. Old English developed from a set of Anglo-Frisian languages, Anglo-Frisian or Ingvaeonic dialects originally spoken by Germanic peoples, Germanic tribes traditionally known as the Angles, Sa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coast To Coast Walk
The Coast to Coast Walk is a long-distance footpath between the west and east coasts of Northern England, nominally long. Devised by Alfred Wainwright, it passes through three contrasting national parks: the Lake District National Park, the Yorkshire Dales National Park, and the North York Moors National Park. The current actual measured distance is reported as . Wainwright recommends that walkers dip their booted feet in the Irish Sea at St Bees and, at the end of the walk, in the North Sea at Robin Hood's Bay. It has been an unofficial and mostly unsignposted trail. However on 12 August 2022 it was announced that the Coast to Coast Walk would become an official National Trail, following a successful campaign by the Wainwright Society (the official Responsible Organisation for the trail). Work will commence to upgrade the route and officially open it in 2025 (at long). History and status The Coast to Coast was originally described by Alfred Wainwright in his 1973 boo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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