Earl Crag
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Earl Crag
Earl Crag is a gritstone crag and climbing area in Craven, North Yorkshire, England. It is home to Lund's Tower, Wainman's Pinnacle, and The Hitching Stone, all of which are near Cowling A cowling is the removable covering of a vehicle's engine, most often found on automobiles, motorcycles, airplanes, and on outboard boat motors. On airplanes, cowlings are used to reduce drag and to cool the engine. On boats, cowlings are a cove .... Climbing Earl Crag itself is popular for climbing and has many different possible routes and climbing techniques. The Hitching Stone Some people climb The Hitching Stone, which is an old gritstone erratic nearby Earl Crag. History Architecture Lund’s Tower Lund's Tower, also known as Sutton Pinnacle, was built by James Lund on Earl Crag in 1887 and designed by R. B. Broster & Sons. Wainman’s Pinnacle Wainman's Pinnacle, also known as Cowling Pinnacle, was built on Earl Crag in 1898 as a memorial to the Napoleonic Wars by ...
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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. ...
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Bradford
Bradford is a city and the administrative centre of the City of Bradford district in West Yorkshire, England. The city is in the Pennines' eastern foothills on the banks of the Bradford Beck. Bradford had a population of 349,561 at the 2011 census; the second-largest population centre in the county after Leeds, which is to the east of the city. It shares a continuous built-up area with the towns of Shipley, Silsden, Bingley and Keighley in the district as well as with the metropolitan county's other districts. Its name is also given to Bradford Beck. It became a West Riding of Yorkshire municipal borough in 1847 and received its city charter in 1897. Since local government reform in 1974, the city is the administrative centre of a wider metropolitan district, city hall is the meeting place of Bradford City Council. The district has civil parishes and unparished areas and had a population of , making it the most populous district in England. In the century leadin ...
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Gritstone
Gritstone or grit is a hard, coarse-grained, siliceous sandstone. This term is especially applied to such sandstones that are quarried for building material. British gritstone was used for millstones to mill flour, to grind wood into pulp for paper and for grindstones to sharpen blades. "Grit" is often applied to sandstones composed of angular sand grains. It may commonly contain small pebbles. " Millstone Grit" is an informal term for a succession of gritstones which are to be found in the Pennines (including the Peak District) of northern England. These sediments were laid down in the late (upper) Paleozoic era, in the Carboniferous period, in deltaic conditions. The Millstone Grit Group is a formal stratigraphic term for this sequence of rocks. The gritstone edges of the Peak District are an important climbing area and the rock is much relished by English climbers, among whom it has almost cult status and is often referred to as "God's own rock". The rough surface provide ...
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Crag
Crag may refer to: * Crag (climbing), a cliff or group of cliffs, in any location, which is or may be suitable for climbing * Crag (dice game), a dice game played with three dice * Crag, Arizona, US * Crag, West Virginia, US * Crag and tail, a geological formation caused by the passage of a glacier over an area of hard rock * Crag Group, a geological group outcropping in East Anglia, UK ** Coralline Crag Formation ** Norwich Crag Formation ** Red Crag Formation ** Wroxham Crag Formation, see Cromer Forest Bed * Crag Hotel, Penang, Malaysia * Crag Jones (born 1962), Welsh climber * USS ''Crag'' (AM-214), a 1943 US Navy ''Admirable''-class minesweeper * The Crag, the final event in the Nickelodeon Guts action sports program * Club de Radioaficionados de Guatemala, an amateur radio organization in Guatemala * Constitutional Reform and Governance Act 2010 The Constitutional Reform and Governance Act 2010 (c. 25), or CRAG Act, is an Act of the Parliament of the United Kingdom on ...
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Climbing Area
A climbing area is a small geographical region with a concentration of opportunities for climbing. The term is most commonly used of rock climbing areas, but there are also ice climbing areas that have the right combination of steepness and water to result in climbable ice during the winter. While there are many mountains and cliffs in the world, only a small percentage are popular for climbing. Mountain ranges are frequently at high elevations, remote, and tend to have poor weather much of the time, which means that the climber spends more time hiking, camping, and battling the elements than actually climbing. At the opposite end of the scale, many cliffs are too small or the rock is too unstable to make for an enjoyable and safe experience. Characteristics An ideal climbing area has these qualities: * Close to an access road * Large number of different routes * Solid and stable rock * Safe descent routes * Good weather * Free access * Uncrowded Development of a climbing ar ...
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Craven In The Domesday Book
The extent of the medieval district of Craven, in the north of England is a matter of debate. The name Craven is either pre-Celtic Britain, Britonnic or Romano-British in origin. However, its usage continued following the ascendancy of the Anglo-Saxons and the Normans – as was demonstrated by its many appearances in the Domesday Book of 1086. Places described as being ''In Craven'' in the Domesday Book fell later within the modern county of North Yorkshire, as well as neighbouring areas of West Yorkshire, Lancashire and Cumbria. Usage of Craven in the Domesday Book is, therefore, circumstantial evidence of an extinct, British or Anglo-Saxon kingdom or subnational entity (such as a shire or earldom). The modern local government district of Craven – a much smaller area entirely within North Yorkshire – was defined in 1974. Background Although historic Craven extended a little further southeast in Yorkshire, as it still does with the Church of England's Deanery of ...
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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 ...
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Lund's Tower
Lund's Tower is a stone-built folly situated to the south-west of the North Yorkshire village of Sutton-in-Craven. It is also known as Cowling Pinnacle, Sutton Pinnacle, the Ethel Tower, the Jubilee Tower or, in conjunction with the nearby Wainman's Pinnacle, the pair are referred to as the Salt and Pepper Pots. It is listed in the National Heritage List for England at Grade II. History James Lund (1829–1903) commissioned the Keighley architectural firm of R. B. Broster & Sons to design the tower, which was built in 1887. Different reasons have been given for why Lund wanted the folly built: local residents refer to it as the Ethel Tower, believing it was constructed either to celebrate the birth of Lund's daughter Ethel – or her 21st birthday; others refer to it as the Jubilee Tower, believing it commemorated the 1887 jubilee of Queen Victoria. It is also known as Sutton Pinnacle. Lund was the son of William Lund, the owner of William Lund & Son, a large textile manufactu ...
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Wainman's Pinnacle
Wainman's Pinnacle, originally built as a folly (and still used as a folly), is a stone obelisk in Sutton-in-Craven, North Yorkshire. It tends to be referred to as ‘Cowling Pinnacle’ or 'The Salt Pot' and could also be seen as being a part of the village of Cowling. It has been a grade II listed building in the National Heritage List for England since 23 October 1984. Wainman’s Pinnacle is situated upon Earl Crag and is often associated with Lund’s Tower as they are both locally known as the Salt and Pepper Pots. History Wainman’s Pinnacle was built in 1898 as a memorial to the Napoleonic Wars The Napoleonic Wars (1803–1815) were a series of major global conflicts pitting the French Empire and its allies, led by Napoleon I, against a fluctuating array of European states formed into various coalitions. It produced a period of Fren ... by a man known as Wainman, and is thought to have been designed by R. B. Broster & Sons. It was rebuilt in 1900 by locals ...
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The Hitching Stone
The Hitching Stone is a gritstone erratic block on Keighley Moor, North Yorkshire, near Earl Crag and the village of Cowling. It is very close to the border between North Yorkshire and West Yorkshire and the border between Yorkshire and Lancashire. It is said to be the largest boulder in Yorkshire at long, wide and high. It is also said to weigh a lot more than 1000 tonnes. Geography The Hitching Stone is from the town of Keighley and is at an elevation of . History The Hitching Stone and all the other erratic boulders on Keighley Moor were put in place thousands to possibly millions of years ago during the Pleistocene Epoch. The Hitching Stone most likely originally came from Earl Crag during this time. As a result of the fact that The Hitching Stone lies at the borders of historic counties, ancient councils and parliaments met at the stone and markets, fair A fair (archaic: faire or fayre) is a gathering of people for a variety of entertainment or commercial ...
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Cowling, Craven
Cowling is a village, electoral division and civil parish in the Craven district of North Yorkshire, England. It is situated on the borders with the adjacent counties of West Yorkshire, and Lancashire. Historically part of the West Riding of Yorkshire, it is a village consisting of 2,000 to 3,000 residents, measured at 2,355 in the Census 2011. The village is expanding due to new housing being built in the middle of the village. Cowling includes a variety of services to support the community including a village hall, primary school, shops, a pub, a restaurant, a pizza take-away, and hairdressers. A gala is held in Cowling every year. History The village is Saxon in origin and is recorded in the ''Domesday Book'' as 'Collinge'. The name means Coll's people or tribe. At the time of the Norman conquest the main landowner was Gamel who had very large land holdings in Yorkshire. His name survives in Gamsgill on the northern edge of the village. Originally the village comprised t ...
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Mountains And Hills Of North Yorkshire
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain ...
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