|
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 th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Strid
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 th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Grassington
Grassington is a market town and civil parish in the Craven district of North Yorkshire, England. The population of the parish at the 2011 Census was 1,126. Historically part of the West Riding of Yorkshire, the town is situated in Wharfedale, about north-west from Bolton Abbey, and is surrounded by limestone scenery. Nearby villages include Linton, Threshfield, Hebden, Conistone and Kilnsey. History The Domesday Book lists Grassington as part of the estate of Gamal Barn including 7 carucates of ploughland (840 acres/350ha) including Grassington, Linton and Threshfield. The Norman conquest of England made it part of the lands of Gilbert Tison. But, by 1118, Tison had suffered a demotion and his lands returned to the king before being given to Lord Percy. Originally the settlement was spelt as Gherinstone and also was documented as Garsington or Gersington. The name Grassington derives variously from the Scandinavian, Anglo-Saxon and Gothic languages, and means eit ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tadcaster
Tadcaster is a market town and civil parish in the Selby district of North Yorkshire, England, east of the Great North Road, 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 near Cawood. Tadcaster is twinned with Saint-Chély-d'Apcher in France. The town was part of the West Riding of Yorkshire until 1974, but is now part of North Yorkshire. Thanks to its position on the banks of the River Wharfe parts of the town adjacent to the bridge are prone to flooding. History Roman The 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 which continues and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Appletreewick
Appletreewick is a village and civil parish in the Craven district of North Yorkshire, England, north-east of Skipton, from Skipton railway station and from Leeds Bradford International Airport. Appletreewick is in Wharfedale in the Yorkshire Dales, a popular place for visitors, especially in the summer months, on the banks of the River Wharfe. The civil parish includes the hamlet of Skyreholme and the western end of the village of Greenhow. The parish also includes Parcevall Hall, Stump Cross Caverns, the eastern part of Grimwith Reservoir and extensive areas of moorland north and east of the village. Barden Fell is a grouse moor belonging to the Bolton Abbey Estate, and Simon's Seat is a prominent rock outcrop to the north of Barden Fell. The civil parish had a population of 218 at the 2011 Census. History The village is mentioned in the Domesday Book and its name is derived from the Old English of ''æppel-trēow wīc'', which means the ''Apple-tree specialis ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Conistone
Conistone is a small village in the Craven district of North Yorkshire, England. It lies north of Grassington, south of Kettlewell and north of Skipton beside the River Wharfe, in Upper Wharfedale. History Conistone is mentioned in the Domesday Book as ''Cunestune'' and belonging to Ketil. The name derives from a mix of Old Danish (''Kunung'') and Old English (''tūn''), which means King's farm or Settlement. The village is set in characteristic limestone scenery, including Mossdale Caverns, the dry gorge of Conistone Dib and the limestone outcrop of Conistone Pie. Above the Dib the Dales Way path connects Kettlewell, to its north, and Grassington, to its south, providing distant views over Wharfedale. From the B6160 road, the Wharfe is crossed at Conistone by a stone-arch bridge, which is within easy walking distance of Kilnsey, with its Crag. The parish church, St Mary's Church, dates from the 11th or 12th century, and is a Grade II listed building. Conistone w ... [...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 Norman 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 until the Sportsman Inn at Cowgill i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Yockenthwaite
Yockenthwaite is a hamlet in the Craven district of North Yorkshire, England. It lies in the Langstrothdale valley in the Yorkshire Dales National Park. Historically part of the West Riding of Yorkshire, 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 via road transport. Yockenthwaite stone circle Just to the west of the village by Yockenthwaite Cave, are some ancient stones arranged in a circle. The stones, which are now a scheduled monument, are in diameter and believed to be Bronze Age in origin. The overall s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Wharfe, Wetherby
A river is a natural flowing watercourse, usually freshwater, flowing towards an ocean, sea, lake or another river. In some cases, a river flows into the ground and becomes dry at the end of its course without reaching another body of water. Small rivers can be referred to using names such as creek, brook, rivulet, and rill. There are no official definitions for the generic term river as applied to geographic features, although in some countries or communities a stream is defined by its size. Many names for small rivers are specific to geographic location; examples are "run" in some parts of the United States, "burn" in Scotland and northeast England, and "beck" in northern England. Sometimes a river is defined as being larger than a creek, but not always: the language is vague. Rivers are part of the water cycle. Water generally collects in a river from precipitation through a drainage basin from surface runoff and other sources such as groundwater recharge, sprin ... [...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) 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. ''Fundamentals ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Middle Welsh
Middle Welsh ( cy, Cymraeg Canol, wlm, Kymraec) is the label attached to the Welsh language of the 12th to 15th centuries, of which much more remains than for any earlier period. This form of Welsh developed directly from Old Welsh ( cy, Hen Gymraeg). Literature and history Middle Welsh is the language of nearly all surviving early manuscripts of the ''Mabinogion'', although the tales themselves are certainly much older. It is also the language of most of the manuscripts of Welsh law. Middle Welsh is reasonably intelligible, albeit with some work, to a modern-day Welsh speaker. Phonology The phonology of Middle Welsh is quite similar to that of modern Welsh, with only a few differences. The letter ''u'', which today represents in North Western Welsh dialects and in South Welsh and North East Welsh dialects, represented the close central rounded vowel in Middle Welsh. The diphthong ''aw'' is found in unstressed final syllables in Middle Welsh, while in Modern Welsh it has b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Common Brittonic
Common Brittonic ( cy, Brythoneg; kw, Brythonek; br, Predeneg), also known as British, Common Brythonic, or Proto-Brittonic, was a Celtic language spoken in Britain and Brittany. It is a form of Insular Celtic, descended from Proto-Celtic, a theorized parent tongue that, by the first half of the first millennium BC, was diverging into separate dialects or languages. Pictish is linked, likely as a sister language or a descendant branch. Evidence from early and modern Welsh shows that Common Brittonic took a significant amount of influence from Latin during the Roman period, especially in terms related to the church and Christianity. By the sixth century AD, the tongues of the Celtic Britons were more rapidly splitting into Neo-Brittonic: Welsh, Cumbric, Cornish, Breton, and possibly the Pictish language. Over the next three centuries it was replaced in most of Scotland by Scottish Gaelic and by Old English (from which descend Modern English and Scots) throughout most ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
_001.JPG "Click for more on -> Tadcaster")
