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Baugh Fell
Baugh Fell (, or ) is a large, flat-topped hill in the northern Pennines of England. It lies in the north-western corner of the Yorkshire Dales National Park, immediately to the east of the Howgill Fells and to the north of Whernside, the highest of the Yorkshire Three Peaks. Formerly in the West Riding of Yorkshire, since 1974 it has been part of the county of Cumbria. Topography Baugh Fell is bounded by Garsdale to the south and by the valley of the River Rawthey to the west; on the north-eastern side it adjoins Swarth Fell and Wild Boar Fell. The fell sprawls over a wide area, roughly in size, with generally steep slopes on the Garsdale side and gentler slopes to the west. The Rawthey rises high up on the summit plateau (where it is called Rawthey Gill) and initially flows north, before turning south to form the hill's western boundary. The eastern limit of the fell is marked by Grisedale Beck, the main tributary of the Clough River which flows through Garsdale. The sum ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wild Boar Fell
Wild Boar Fell is a mountain in the Yorkshire Dales National Park, on the eastern edge of Cumbria, England. At , it is either the 4th-highest fell in the Yorkshire Dales or the 5th, depending on whether nearby High Seat (2,326 ft) is counted or not. The nearest high point is Swarth Fell which is a ridge about a mile (1½ km) long to the south, at . To the east, on the opposite side of the narrow dale, are High Seat and Hugh Seat. Wild Boar Fell is on the boundary of the civil parishes of Mallerstang and Ravenstonedale. History According to Wainwright the fell gets its name from the wild boar which inhabited the area over 500 years ago. In earlier times, probably up to the mid 19th century, the Millstone Grit, or gritstone, which forms the flat top of the fell, was used for making millstones. Some partly formed millstones can be seen on the eastern flank of the fell — and also on the corresponding western flank of Mallerstang Edge on the opposite side of the dale. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Plateau
In geology and physical geography, a plateau (; ; ), also called a high plain or a tableland, is an area of a highland consisting of flat terrain that is raised sharply above the surrounding area on at least one side. Often one or more sides have deep hills or escarpments. Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, and erosion by water and glaciers. Plateaus are classified according to their surrounding environment as intermontane, piedmont, or continental. A few plateaus may have a small flat top while others have wide ones. Formation Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, Plate tectonics movements and erosion by water and glaciers. Volcanic Volcanic plateaus are produced by volcanic activity. The Columbia Plateau in the north-western United States is an example. They may be formed by upwelling of volcanic magma or extrusion of lava. The un ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Moorland
Moorland or moor is a type of habitat found in upland areas in temperate grasslands, savannas, and shrublands and montane grasslands and shrublands biomes, characterised by low-growing vegetation on acidic soils. Moorland, nowadays, generally means uncultivated hill land (such as Dartmoor in South West England), but also includes low-lying wetlands (such as Sedgemoor, also South West England). It is closely related to heath, although experts disagree on what precisely distinguishes these types of vegetation. Generally, moor refers to highland and high rainfall zones, whereas heath refers to lowland zones which are more likely to be the result of human activity. Moorland habitats mostly occur in tropical Africa, northern and western Europe, and neotropical South America. Most of the world's moorlands are diverse ecosystems. In the extensive moorlands of the tropics, biodiversity can be extremely high. Moorland also bears a relationship to tundra (where the subsoil is permafros ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rights Of Way In England And Wales
In England and Wales, other than in the 12 Inner London London boroughs, boroughs and the City of London, the right of way is a legally protected right of the public to pass and re-pass on specific paths. The law in England and Wales differs from Scots law in that rights of way exist only where they are so designated (or are able to be designated if not already), whereas in Scotland any route that meets certain conditions is rights of way in Scotland, defined as a right of way, and in addition, there is a general presumption of access to the countryside ("right to roam"). Private rights of way or easements also exist (see also Highways in England and Wales). Inner London Definitive maps of public rights of way have been compiled for all of England and Wales, as a result of the National Parks and Access to the Countryside Act 1949, except the 12 Inner London boroughs, which, along with the City of London, were not covered by the Act. Definitive maps exist for the Outer London bo ... [...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] |
Tarn (lake)
A tarn (or corrie loch) is a Proglacial lake, proglacial mountain lake, pond or pool, formed in a cirque excavated by a glacier. A moraine may form a natural dam below a tarn. Etymology The word is toponymy, derived from the Old Norse word ''tjörn'' ("a small mountain lake without tributaries") meaning pond. In parts of Northern England - predominantly Cumbria but also areas of North Lancashire and North Yorkshire - 'tarn' is widely used as the name for small lakes or ponds, regardless of their location and origin (e.g. Talkin Tarn, Urswick Tarn, Malham Tarn). Similarly, in Scandinavian languages, a ''tjern'' or ''tjørn'' (both Norwegian) or ''tjärn'' or ''tärn'' (both Swedish) is a small natural lake, often in a forest or with vegetation closely surrounding it or growing into the tarn. The specific technical use for a body of water in a glacial corrie comes from high number of tarns found in corries in the Lake District, an upland area in Cumbria. Nonetheless, there are ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Eden, Cumbria
The River Eden is a river that flows through the Eden District of Cumbria, England, on its way to the Solway Firth. Etymology The river was known to the Romans as the ''Itouna'', as recorded by the Greek geographer Claudius Ptolemaeus (Ptolemy) in the 2nd century AD. This name derives from the Celtic word ''ituna'', meaning ''water'', or ''rushing''. Thus there is no relation to the biblical Garden of Eden. Course of river The Eden rises in Black Fell Moss, Mallerstang, on the high ground between High Seat, Yorkshire Dales and Hugh Seat. Here it forms the boundary between the counties of Cumbria and North Yorkshire. Two other rivers arise in the same peat bogs here, within a kilometre of each other: the River Swale and River Ure. It starts life as Red Gill Beck, then becomes Hell Gill Beck, before turning north and joining with Ais Gill Beck to become the River Eden. (Hell Gill Force, just before it meets Ais Gill Beck, is the highest waterfall along its journey to the sea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wensleydale
Wensleydale is the dale or upper valley of the River Ure on the east side of the Pennines, one of the Yorkshire Dales in North Yorkshire, England. It is one of only a few Yorkshire Dales not currently named after its principal river, but the older name, Yoredale, can still be seen on some maps and as the Yoredale Series of geological strata. The dale takes its name from the village of Wensley, once its market town. The valley is famous for its cheese, with the main commercial production at Hawes. Also famous are its ales from Theakston Brewery and Black Sheep Brewery in Masham. Most of the dale is within the Yorkshire Dales National Park. Part of lower Wensleydale, below East Witton, is within the Nidderdale Area of Outstanding Natural Beauty. Addlebrough, a fell, dominates the landscape of the upper dale, and Penhill at is prominent in the lower dale. History Wensleydale was the home of one of Yorkshire's most famous clans, the Metcalfes, after they emigrated from ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Blackpool Tower
Blackpool Tower is a tourist attraction in Blackpool, Lancashire, England, which was opened to the public on 14 May 1894. When it opened, Blackpool Tower was the List of tallest buildings in the British Empire and the Commonwealth, tallest man made structure in the British Empire. Inspired by the Eiffel Tower in Paris, it is tall and is the 125th-tallest freestanding tower in the world. Blackpool Tower is also the common name for the Tower Buildings, an entertainment complex in a red-brick three-storey block that comprises the tower, Tower Circus, the Tower Ballroom, and roof gardens, which was designated a Listed building, Grade I listed building in 1973. Background The Blackpool Tower Company was founded by London-based Standard Contract & Debenture Corporation in 1890; it bought an aquarium on Central Promenade with the intention of building a replica Eiffel Tower on the site. John Bickerstaffe, a former mayor of Blackpool, was asked to become chairman of the new company, and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake District
The Lake District, also known as the Lakes or Lakeland, is a mountainous region in North West England. A popular holiday destination, it is famous for its lakes, forests, and mountains (or ''fells''), and its associations with William Wordsworth and other Lake Poets and also with Beatrix Potter and John Ruskin. The Lake District National Park was established in 1951 and covers an area of . It was designated a UNESCO World Heritage Site in 2017. The Lake District is today completely within Cumbria, a county and administrative unit created in 1974 by the Local Government Act 1972. However, it was historically divided between three English counties ( Cumberland, Westmorland and Lancashire), sometimes referred to as the Lakes Counties. The three counties met at the Three Shire Stone on Wrynose Pass in the southern fells west of Ambleside. All the land in England higher than above sea level lies within the National Park, including Scafell Pike, the highest mountain in England. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Trig Point
A triangulation station, also known as a trigonometrical point, and sometimes informally as a trig, is a fixed surveying station, used in geodetic surveying and other surveying projects in its vicinity. The nomenclature varies regionally: they are generally known as trigonometrical stations or triangulation stations in North America, trig points in the United Kingdom, trig pillars in Ireland, trig stations or trig points in Australia and New Zealand, and trig beacons in South Africa. Use The station is usually set up by a government with known coordinates and elevation published. Many stations are located on hilltops for the purposes of visibility. A graven metal plate on the top of a pillar may provide a mounting point for a theodolite or reflector, often using some form of kinematic coupling to ensure reproducible positioning. Trigonometrical stations are grouped together to form a network of triangulation. Positions of all land boundaries, roads, railways, bridges and other ... [...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 series ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
