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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, Yorkshire, River Ouse near Cawood, North Yorkshire, 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 C ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Grassington
Grassington is a town and civil parishes in England, civil parish in North Yorkshire, England. The population of the parish at the 2011 Census was 1,126. The village is situated in Wharfedale, about north-west from Bolton Abbey, and is surrounded by limestone scenery. Nearby villages include Linton, North Yorkshire, Linton, Threshfield, Hebden, North Yorkshire, Hebden, Conistone and Kilnsey. Until 1974 it was part of the West Riding of Yorkshire. From 1974 to 2023 it was part of the district of Craven District, Craven, it is now administered by the unitary North Yorkshire Council. History The Craven in the Domesday Book#The Land of Gilbert Tison in Craven, Domesday Book folio 327, Domesday Book lists Grassington as part of Gamal Barn's estate, including 7 carucates of ploughland (840 acres/350ha) including Grassington, Linton, North Yorkshire, Linton and Threshfield. The Norman conquest of England made it part of the lands of Gilbert Tison. But, by 1118, Tison had suffere ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tadcaster
Tadcaster is a market town and civil parishes in England, civil parish in North Yorkshire, England, north-east of Leeds and south-west of York. Its historical importance from Roman times onward was largely as the lowest road crossing-point on the River Wharfe until the construction of the A64 Tadcaster by-pass some to the south, in 1978. There are two rail crossings downstream of the town before the Wharfe joins the River Ouse, Yorkshire, River Ouse near Cawood. Thanks to its position on the banks of the River Wharfe parts of the town adjacent to the bridge are prone to flooding. The town was part of the West Riding of Yorkshire until 1974, but is now part of North Yorkshire. Tadcaster is town twinning, twinned with Saint-Chély-d'Apcher in France. History Roman The Roman Britain, Romans built a settlement and named it ''Calcaria'' from the Latin word for ''lime'', reflecting the importance of the area's limestone geology as a natural resource for quarrying, an industry ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hubberholme
Hubberholme is an old village in Upper Wharfedale in the Yorkshire Dales, North Yorkshire, England, at the point where Langstrothdale meets Wharfedale. It is quite secluded and the nearest village is Buckden. The village was a favourite place of writer and playwright J.B. Priestley who described it as the ''smallest, pleasantest place in the world''. The churchyard of St Michael and All Angels' Church is the resting place of his ashes. The old inn, The George, is opposite the Church. This is notable for the lit candle that sits on the bar to indicate the pub is open and serving. The tradition dates from distinctive auctions for agricultural land or grazing that are still held in The George. The last bid to be received before the candle extinguished is the winner. The George Pub in Hubberholme opens throughout the year (with the White Lion at Cray and the Buck Inn at Buckden the closest alternative watering holes). After the George Inn, there is no pub on the Dales Way unt ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Yockenthwaite
Yockenthwaite is a hamlet in the county of North Yorkshire, England. It lies in the Langstrothdale valley in the Yorkshire Dales National Park. Yockenthwaite is north of Skipton and south of Hawes. The name of the hamlet is said to derive from ''Eoghan's clearing in a wood''. Yockenthwaite lies on the north bank of the River Wharfe. It is better known than may be expected because a children's television character from '' The Rottentrolls'' takes its name from the hamlet. The hamlet is connected to the road that winds up and down Langstrothdale by a grade II listed bridge from the early 18th century. This is the only route into and out of the hamlet by road. Yockenthwaite Hall is a farmhouse dating from the 18th century. It is a Grade II listed building. Yockenthwaite Bridge is also a Grade II listed building. Until 1974 it was part of the West Riding of Yorkshire. From 1974 to 2023 it was part of the district of Craven, it is now administered by the unitary North Yorksh ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Wharfe, Wetherby
A river is a natural stream of fresh water that flows on land or inside caves towards another body of water at a lower elevation, such as an ocean, lake, or another river. A river may run dry before reaching the end of its course if it runs out of water, or only flow during certain seasons. Rivers are regulated by the water cycle, the processes by which water moves around the Earth. Water first enters rivers through precipitation, whether from rainfall, the runoff of water down a slope, the melting of glaciers or snow, or seepage from aquifers beneath the surface of the Earth. Rivers flow in channeled watercourses and merge in confluences to form drainage basins, or catchments, areas where surface water eventually flows to a common outlet. Rivers have a great effect on the landscape around them. They may regularly overflow their banks and flood the surrounding area, spreading nutrients to the surrounding area. Sediment or alluvium carried by rivers shapes the landscape aro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Meander On The River Wharfe Between Kettlewell And Starbotton (12th February 2013)
A meander is one of a series of regular sinuous curves in the channel of a river or other watercourse. It is produced as a watercourse erodes the sediments of an outer, concave bank ( cut bank or river cliff) and deposits sediments on an inner, convex bank which is typically a point bar. The result of this coupled erosion and sedimentation is the formation of a sinuous course as the channel migrates back and forth across the axis of a floodplain. The zone within which a meandering stream periodically shifts its channel is known as a meander belt. It typically ranges from 15 to 18 times the width of the channel. Over time, meanders migrate downstream, sometimes in such a short time as to create civil engineering challenges for local municipalities attempting to maintain stable roads and bridges.Neuendorf, K.K.E., J.P. Mehl Jr., and J.A. Jackson, J.A., eds. (2005) ''Glossary of Geology'' (5th ed.). Alexandria, Virginia, American Geological Institute. 779 pp. Charlton, R., 2007. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Andrew Breeze
Andrew Breeze FRHistS FSA (born 1954), has been professor of philology at the University of Navarra since 1987. Early life Breeze was born in 1954 and educated at Sir Roger Manwood's School, Emmanuel College, Cambridge (where he took a first in English in 1974 and in Anglo-Saxon, Norse and Celtic in 1976, and his PhD in 1992), and at St John's College, Oxford (where he took a diploma in Celtic studies in 1978). In 1986, he worked as a scholar for the Dublin Institute for Advanced Studies at the school of Celtic Studies. He is married with six children. Work Besides numerous research papers on the philology of many Celtic languages, he is the author of ''Medieval Welsh Literature'' (1997) and ''The Origins of the "Four Branches of the Mabinogi"'' (2009). He is also co-author with Richard Coates of ''Celtic Voices, English Places'' (2000). Breeze has written about Mabinogi studies, and '' The Mabinogion'' research, especially addressing historical and political parall ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Patrick Sims-Williams
Patrick Sims-Williams is Emeritus Professor of Celtic Studies at Aberystwyth University and founding editor of the journal '' Cambrian Medieval Celtic Studies''. Education Sims-Williams was educated at Borden Grammar School in Sittingbourne, Kent. He took a B.A. at Trinity Hall, Cambridge, achieving upper-second-class honours in the Anglo-Saxon, Norse and Celtic tripos in 1972, followed by a PhD at the University of Birmingham. His twin brother Nicholas Sims-Williams is a scholar of Central Asia. Career Following the early retirement of the Celticist Rachel Bromwich from Cambridge's Department of Anglo-Saxon, Norse and Celtic at the end of 1976, Sims-Williams was appointed to a University Assistant Lectureship in the Department from the beginning of 1977.Michael Lapidge, 'Introduction', in ''H. M. Chadwick and the Study of Anglo-Saxon, Norse and Celtic in Cambridge'', ed. by Michael Lapidge, ''Cambrian Medieval Celtic Studies'', 69/70 (2015) , pp. 1–58. He was promoted to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Root (linguistics)
A root (also known as a root word or radical) is the core of a word that is irreducible into more meaningful elements. In morphology, a root is a morphologically simple unit which can be left bare or to which a prefix or a suffix can attach. The root word is the primary lexical unit of a word, and of a word family (this root is then called the base word), which carries aspects of semantic content and cannot be reduced into smaller constituents. Content words in nearly all languages contain, and may consist only of, root morphemes. However, sometimes the term "root" is also used to describe the word without its inflectional endings, but with its lexical endings in place. For example, ''chatters'' has the inflectional root or lemma ''chatter'', but the lexical root ''chat''. Inflectional roots are often called stems. A root, or a root morpheme, in the stricter sense, is a mono-morphemic stem. The traditional definition allows roots to be either free morphemes or bound ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Proto-Indo-European
Proto-Indo-European (PIE) is the reconstructed common ancestor of the Indo-European language family. No direct record of Proto-Indo-European exists; its proposed features have been derived by linguistic reconstruction from documented Indo-European languages. Far more work has gone into reconstructing PIE than any other proto-language, and it is the best understood of all proto-languages of its age. The majority of linguistic work during the 19th century was devoted to the reconstruction of PIE and its daughter languages, and many of the modern techniques of linguistic reconstruction (such as the comparative method) were developed as a result. PIE is hypothesized to have been spoken as a single language from approximately 4500 BCE to 2500 BCE during the Late Neolithic to Early Bronze Age, though estimates vary by more than a thousand years. According to the prevailing Kurgan hypothesis, the proto-Indo-European homeland, original homeland of the Proto-Indo-Europeans may ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
