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Clough River
The Clough River is a river in Cumbria, England. A tributary of the River Rawthey, it flows for primarily through the Garsdale valley. Course The river rises at Grisedale in south-eastern Cumbria, where a group of smaller streams draining Grisedale Pike converge as Grisedale Beck. The young Clough River then goes through a short valley (Grisedale, "The Dale That Died"), and over a waterfall before being named Clough at Clough Farm, Garsdale Head, where it enters Garsdale, a valley formed by the river between Baugh Fell (to the north) and Rise Hill (to the south). The Clough is mainly shallow and rocky, with occasional pools large enough for swimming, though the water is always cold. The A684 (Northallerton to Kendal) road follows the river for seven miles with frequent bridges in the upper part of the dale. At Longstone Fell the main (former turnpike) road rises to a well-known view-point looking over the Howgill Fells, and the river descends to Danny Bridge, the site of a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Garsdale Head
Garsdale Head is a hamlet mainly within the South Lakeland district of Cumbria, England. Historically part of the West Riding of Yorkshire, the hamlet is now on the border with Richmondshire, North Yorkshire. It lies within the boundaries of the Yorkshire Dales National Park. Garsdale Head is mainly within the civil parish and valley of Garsdale, and on the A684 road between Sedbergh, approximately to the west (ten miles by road), and Hawes, to the east. The hamlet's chief landmark is Garsdale railway station on the Settle to Carlisle and Wensleydale Railways. Until the branch line to Hawes was closed in 1964 the alternative name for Garsdale Head was Hawes Junction, a name which remains in common use. Sixteen cottages were built by the Midland Railway Company for its employees soon after the opening of the line in 1876. Another six "Moorcock Cottages" were built in similar Victorian style half a mile away over the border in Richmondshire. Just before the border, in a mat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 derived from ''*lǭn'' meaning "full, abundant", or "healthy, pure" (c.f. Old Irish ''slán'', Welsh ''llawn''). Secondly, ''Lune'' may represent Old English ''Ēa Lōn'' (''ēa'' = "river") as a phonetic adaptation of a Romano-British name referring to a Romano-British god Ialonus who was worshipped in the area. Springs The river begins as a stream at Newbiggin, in the parish of Ravenstonedale, Cumbria, at St. Helen's Well (elevation of above sea level) and some neighbouring springs. On the first two miles of its course, it is joined by four streams, two of them as short as itself, but two much longer. These are the Bessy Beck (short), the Dry Beck of 4.9 kilometres' (three miles) length at from St. Helen's Well, the Sandwath Bec ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Rivers Of England
This is a list of rivers of England, organised geographically and taken anti-clockwise around the English coast where the various rivers discharge into the surrounding seas, from the Solway Firth on the Scottish border to the Welsh Dee on the Welsh border, and again from the Wye on the Welsh border anti-clockwise to the Tweed on the Scottish border. Tributaries are listed down the page in an upstream direction, i.e. the first tributary listed is closest to the sea, and tributaries of tributaries are treated similarly. Thus, in the first catchment below, the River Sark is the lowermost tributary of the Border Esk and the Hether Burn is the lowermost tributary of the River Lyne. The main stem (or principal) river of a catchment is labelled as (MS), left-bank tributaries are indicated by (L), right-bank tributaries by (R). Note that in general usage, the 'left (or right) bank of a river' refers to the left (or right) hand bank, as seen when looking downstream. Where a named river ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
South Lakeland
South Lakeland is a local government district in Cumbria, England. The population of the non-metropolitan district was 102,301 according to the 2001 census, increasing to 103,658 at the 2011 Census. Its council is based in Kendal. It includes much of the Lake District as well as northwestern parts of the Yorkshire Dales. The district was created on 1 April 1974 under the Local Government Act 1972. It was formed from the Kendal borough, Windermere urban district, most of Lakes urban district, South Westmorland Rural District, from Westmorland, Grange and Ulverston urban districts and North Lonsdale Rural District from Lancashire, and Sedbergh Rural District from the West Riding of Yorkshire. In July 2021 the Ministry of Housing, Communities and Local Government announced that in April 2023, Cumbria will be reorganised into two unitary authorities. South Lakeland District Council is to be abolished and its functions transferred to a new authority, to be known as W ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Yorkshire Dales National Park
The Yorkshire Dales National Park is a national park in England covering most of the Yorkshire Dales. Most of the park is in North Yorkshire, with a sizeable area in Westmorland (Cumbria) and a small part in Lancashire. The park was designated in 1954, and extended in 2016. Over 95% of the land in the Park is under private ownership; there are over 1,000 farms in this area. In late 2020, the park was named as an International Dark Sky Reserve. This honour confirms that the area has "low levels of light pollution with good conditions for astronomy". Some 23,500 residents live in the park (as of 2017); a 2018 report estimated that the Park attracted over four million visitors per year. The economy consists primarily of tourism and agriculture. Location The park is north-east of Manchester; Otley, Ilkley, Leeds and Bradford lie to the south, while Kendal is to the west, Darlington to the north-east and Harrogate to the south-east. The national park does not include al ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
West Riding Of Yorkshire
The West Riding of Yorkshire is one of three historic subdivisions of Yorkshire, England. From 1889 to 1974 the administrative county County of York, West Riding (the area under the control of West Riding County Council), abbreviated County of York (WR), was based closely on the historic boundaries. The lieutenancy at that time included the City of York and as such was named West Riding of the County of York and the County of the City of York. Its boundaries roughly correspond to the present ceremonial counties of West Yorkshire, South Yorkshire and the Craven, Harrogate and Selby districts of North Yorkshire, along with smaller parts in Lancashire (for example, the parishes of Barnoldswick, Bracewell, Brogden and Salterforth became part of the Pendle district of Lancashire and the parishes of Great Mitton, Newsholme and Bowland Forest Low became part of the Ribble Valley district also in Lancashire), Cumbria, Greater Manchester and, since 1996, the unitary East Riding ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dent Fault
The Dent Fault is a major fault zone on the boundary between the counties of Cumbria and North Yorkshire in northern England. It is named after the village of Dent in Dentdale, on the western margin of the Yorkshire Dales. The fault, or rather the 'Dent Fault System' – a collection of closely associated faults and folds, defines the western edge of the Askrigg Block, a geological structure that underlies the Yorkshire Dales. The fault is associated with the Taythes Anticline to its west and the Fell End Syncline to its east. Other than vertical movement on the fault, there has also been an element of strike-slip movement. To the north, the fault links with the Pennine Fault System in the vicinity of Brough and with the Craven Fault System near Kirkby Lonsdale to the south.Stone et al. 2010 ''British Regional Geology: Northern England'' (5th edition) Keyworth, Notts, British Geological Survey Regional setting The Carboniferous geology of northern England consists of a s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Adam Sedgwick
Adam Sedgwick (; 22 March 1785 – 27 January 1873) was a British geologist and Anglican priest, one of the founders of modern geology. He proposed the Cambrian and Devonian period of the geological timescale. Based on work which he did on Welsh rock strata, he proposed the Cambrian period in 1835, in a joint publication in which Roderick Murchison also proposed the Silurian period. Later in 1840, to resolve what later became known as the Great Devonian Controversy about rocks near the boundary between the Silurian and Carboniferous periods, he and Murchison proposed the Devonian period. Though he had guided the young Charles Darwin in his early study of geology and continued to be on friendly terms, Sedgwick was an opponent of Darwin's theory of evolution by means of natural selection. He strongly opposed the admission of women to the University of Cambridge, in one conversation describing aspiring female students as "nasty forward minxes." Life and career Sedgwick ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sedbergh
Sedbergh ( or ) is a town and civil parish in Cumbria, England. The 2001 census gave the parish a population of 2,705, increasing at the 2011 census to 2,765. Historically in the West Riding of Yorkshire, it lies about east of Kendal, north of Lancaster and about north of Kirkby Lonsdale, just within the Yorkshire Dales National Park. It stands at the foot of Howgill Fells, on the north bank of the River Rawthey, which joins the River Lune below the town. Situation Sedbergh has a narrow main street lined with shops. From all angles, the hills rising behind the houses can be seen. Until the coming of the Ingleton Branch Line in 1861, these remote places were reachable only by walking over some steep hills. The line to Sedbergh railway station ran from 1861 to 1954. The civil parish covers a large area, including the hamlets of Millthrop, Catholes, Marthwaite, Brigflatts, High Oaks, Howgill, Lowgill and Cautley, the southern part of the Howgill Fells and the western p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
England
England is a country that is part of the United Kingdom. It shares land borders with Wales to its west and Scotland to its north. The Irish Sea lies northwest and the Celtic Sea to the southwest. It is separated from continental Europe by the North Sea to the east and the English Channel to the south. The country covers five-eighths of the island of Great Britain, which lies in the North Atlantic, and includes over 100 smaller islands, such as the Isles of Scilly and the Isle of Wight. The area now called England was first inhabited by modern humans during the Upper Paleolithic period, but takes its name from the Angles, a Germanic tribe deriving its name from the Anglia peninsula, who settled during the 5th and 6th centuries. England became a unified state in the 10th century and has had a significant cultural and legal impact on the wider world since the Age of Discovery, which began during the 15th century. The English language, the Anglican Church, and Engli ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Waterfall
A waterfall is a point in a river or stream where water flows over a vertical drop or a series of steep drops. Waterfalls also occur where meltwater drops over the edge of a tabular iceberg or ice shelf. Waterfalls can be formed in several ways, but the most common method of formation is that a river courses over a top layer of resistant bedrock before falling on to softer rock, which erodes faster, leading to an increasingly high fall. Waterfalls have been studied for their impact on species living in and around them. Humans have had a distinct relationship with waterfalls for years, travelling to see them, exploring and naming them. They can present formidable barriers to navigation along rivers. Waterfalls are religious sites in many cultures. Since the 18th century they have received increased attention as tourist destinations, sources of hydropower, andparticularly since the mid-20th centuryas subjects of research. Definition and terminology A waterfall is genera ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stream
A stream is a continuous body of surface water flowing within the bed and banks of a channel. Depending on its location or certain characteristics, a stream may be referred to by a variety of local or regional names. Long large streams are usually called rivers, while smaller, less voluminous and more intermittent streams are known as streamlets, brooks or creeks. The flow of a stream is controlled by three inputs – surface runoff (from precipitation or meltwater), daylighted subterranean water, and surfaced groundwater ( spring water). The surface and subterranean water are highly variable between periods of rainfall. Groundwater, on the other hand, has a relatively constant input and is controlled more by long-term patterns of precipitation. The stream encompasses surface, subsurface and groundwater fluxes that respond to geological, geomorphological, hydrological and biotic controls. Streams are important as conduits in the water cycle, instruments in groundw ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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