Pennine Hills
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Pennine Hills
The Pennines (), also known as the Pennine Chain or Pennine Hills, are a range of uplands mainly located in Northern England. Commonly described as the "backbone of England" because of its length and position, the range runs from Derbyshire and Staffordshire in the North Midlands, north of the Midlands to Northumberland in North East England. From the River Tyne, Tyne Gap in the north, the range extends south through the North Pennines, Yorkshire Dales, South Pennines, and Peak District to end near the valley of the River Trent. The Border Moors & Forests, Border Moors and Cheviot Hills, which lie beyond the Tyne Gap, are included in some definitions of the range. The range is divided into two by the Aire Gap, a wide pass formed by the valleys of the rivers River Aire, Aire and River Ribble, Ribble. There are several Spur (topography), spurs off the main Pennine range east into Greater Manchester and Lancashire, comprising the Rossendale Valley, Rossendale Fells, West Pennine Mo ...
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United Kingdom
The United Kingdom of Great Britain and Northern Ireland, commonly known as the United Kingdom (UK) or Britain, is a country in Northwestern Europe, off the coast of European mainland, the continental mainland. It comprises England, Scotland, Wales and Northern Ireland. The UK includes the island of Great Britain, the north-eastern part of the island of Ireland, and most of List of islands of the United Kingdom, the smaller islands within the British Isles, covering . Northern Ireland shares Republic of Ireland–United Kingdom border, a land border with the Republic of Ireland; otherwise, the UK is surrounded by the Atlantic Ocean, the North Sea, the English Channel, the Celtic Sea and the Irish Sea. It maintains sovereignty over the British Overseas Territories, which are located across various oceans and seas globally. The UK had an estimated population of over 68.2 million people in 2023. The capital and largest city of both England and the UK is London. The cities o ...
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North East England
North East England, commonly referred to simply as the North East within England, is one of nine official regions of England. It consists of County DurhamNorthumberland, , Northumberland, Tyne and Wear and part of northern North Yorkshire. It is the least-populated region of England: home to 2.6 million residents in 2022. The largest settlements are Newcastle upon Tyne, Middlesbrough, Sunderland, Gateshead, Darlington, Hartlepool and Durham, England, Durham. The North East is covered by two mayoral combined authorities, North East Combined Authority and Tees Valley Combined Authority. It is one of three regions, the other two being North West England and Yorkshire and the Humber, that make up Northern England. History The region's historic importance is displayed by Northumberland's ancient castles, the two World Heritage Sites of Durham Cathedral and Durham Castle, and Hadrian's Wall, one of the frontiers of the Roman Empire. In fact, Roman archaeology can be found widely ...
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Rossendale Valley
The Rossendale Valley is in the Rossendale area of Lancashire, England, between the West Pennine Moors and the main range of the Pennines. The area includes the steep-sided valleys of the River Irwell and its tributaries (between Rawtenstall and Bacup), which flow southwards into Greater Manchester. The rivers cut through the moorland of the Rossendale Hills, generally characterized by open unwooded land, despite the ancient designation of "forest". History One of the earliest sites of historical interest in the valley is that of the dykes at Broadclough, which are associated with the Battle of Brunanburh. In late Middle Ages, the valley was part of the Royal Forest of Rossendale. The original medieval meaning of 'forest' was similar to a 'preserve', for example land that is legally kept for specific purposes such as royal hunting. So 'forests' were areas large enough to support species such as wolves and deer for game hunting and they encompassed other habitats such as he ...
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Spur (topography)
A spur is a lateral ridge or tongue of land descending from a hill, mountain or main crest of a ridge. It can also be defined as another hill or mountain range which projects in a lateral direction from a main hill or mountain range. Examples of spurs include: * Abbott Spur, which separates the lower ends of Rutgers Glacier and Allison Glacier on the west side of the Royal Society Range in Victoria Land, Antarctica * Boott Spur, a subpeak of Mount Washington * Kaweah Peaks Ridge, a spur of the Great Western Divide, a sub-range of California's Sierra Nevada * Kelley Spur, east of Spear Spur on the south side of Dufek Massif in the Pensacola Mountains, Antarctica * Geneva Spur on Mount Everest * Sperrin Mountains in Northern Ireland''Golden Light in the Sperrins, ...
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River Ribble
The River Ribble runs through North Yorkshire and Lancashire in Northern England. It starts close to the Ribblehead Viaduct in North Yorkshire, and is one of the few that start in the Yorkshire Dales and flow westwards towards the Irish Sea (the Dee in Dentdale and the Twiss in Kingsdale being notable others). Etymology The name ''Ribble'' may be a Brittonic compound-formation. The second element is the noun ''*pol'', with connotations including "puddle, pond, upland-stream" ( Welsh ''pwll''). The first is ''rö-'', an intensive prefix, with nouns meaning "great" (Welsh ''rhy-'', Cornish re-). Ribble may once have been known as ''*Bremetonā-'', underlying the name ''Bremetenacum'', the Roman fort at Ribchester. Involved here is the Brittonic root ''*breμ–'', meaning "roaring" (cf. Welsh ''brefu''), as observed at the river-names Breamish in Northumberland, Braan in Scotland and Brefi in Wales. History Neolithic to Saxon finds from along the River Ribble during th ...
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River Aire
The River Aire is a major river in Yorkshire, England, in length. Part of the river below Leeds is canalised, and is known as the Aire and Calder Navigation. The ''Handbook for Leeds and Airedale'' (1890) notes that the distance from Malham to Howden is direct, but the river's meanderings extend that to . Between Malham Tarn and Airmyn, the river drops . Course The Aire starts at Malham Tarn and becomes a subterranean stream at 'Water Sinks' about one mile (1.6 km) before the top of Malham Cove, it then flows underground to Aire Head, just below Malham, in North Yorkshire, and then flows through Gargrave and Skipton. After Cononley, the river enters West Yorkshire where it passes through the former industrial areas of Keighley, Bingley, Saltaire and Shipley. It then passes through Leeds and on to Swillington and Woodlesford. At Castleford is the confluence of the Aire and Calder; just downstream of the confluence was the ford where the ancient British road, us ...
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Aire Gap
Aire Gap is a pass through the Pennines in England formed by geologic fault (geology), faults and carved out by glaciers. The term is used to describe a geological division, a travel route, or a location that is an entry into the Aire river valley. Geology Geologically the Aire Gap lies between the Craven Fault and the limestone uplands of the Yorkshire Dales to the north and the Forest of Bowland and the millstone grit moors of the South Pennines. The South Pennines is the system between the Aire Gap and the Peak District.Encyclopædia Britannica The gap was formed by the dropping of the Craven Faults in the Carboniferous through Jurassic periods combined with glacial scouring by ice sheets in the Pleistocene Ice Age. The Aire Gap splits the Pennines into north and south by allying with the River Ribble. The Pennine chain is divided into two sections by the Aire Gap formed by the River Aire flowing south, a member of the Humber basin, and the Ribble flowing west and entering th ...
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Cheviot Hills
The Cheviot Hills (), or sometimes The Cheviots, are a range of uplands straddling the Anglo-Scottish border between Northumberland and the Scottish Borders. The English section is within the Northumberland National Park. The range includes The Cheviot (the highest hill), plus Hedgehope Hill to the east, Windy Gyle to the west, and Cushat Law and Bloodybush Edge to the south. The hills are sometimes considered a part of the Southern Uplands of Scotland as they adjoin the uplands to the north. Since the Pennine Way runs through the region, the hills are also considered a part of the northern Pennines although they are separated from the Cheviot Hills by the Tyne Gap, part of which lies within the southern extent of the Northumberland National Park. The Cheviot Hills are primarily associated with geological activity from approximately 480 to 360 million years ago, when the continents of Avalonia and Laurentia collided, resulting in extensive volcanic activity (the Caledonia ...
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Border Moors & Forests
Border Moors and Forests NCA is an upland plateau region in Northern England between the North East and North West regions, and touching the Anglo-Scottish border. The region, like much of the northern English uplands, is sparsely populated, with scattered farming and hardy shepherding in river valleys. Because of this sparse population, 39% of the region is part of the Northumberland National Park in the southeast and several military assets are placed here, both modern and ancient. The NCA is of lower elevation to the Cheviot Hills to the east. The A68 is the only main road going through the region. Conifer plantations, moorland, bogs, wet heaths make up the landscape of the region, which only allows for rough grazing of sheep in most areas outside of the valleys. Afforestation is a major environmental factor within the 20th and 21st centuries, as the Kielder Forest is the largest planted forest in northern Europe and has destroyed many native mires and peat bogs of the region. ...
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River Trent
The Trent is the third Longest rivers of the United Kingdom, longest river in the United Kingdom. Its Source (river or stream), source is in Staffordshire, on the southern edge of Biddulph Moor. It flows through and drains the North Midlands into the Humber Estuary. The river is known for dramatic flooding after storms and spring snowmelt, which in the past often caused the river to change course. The river passes through Stoke-on-Trent, Stone, Staffordshire, Rugeley, Burton-upon-Trent and Nottingham before joining the River Ouse, Yorkshire at Trent Falls to form the Humber Estuary, which empties into the North Sea between Kingston upon Hull in Yorkshire and Immingham in Lincolnshire. The wide Humber estuary has often been described as the boundary between the Midlands and the north of England. Name The name "Trent" is possibly from a Romano-British word meaning "strongly flooding". More specifically, the name may be a contraction of two Romano-British words, ''tros'' ("over" ...
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Peak District
The Peak District is an Highland, upland area in central-northern England, at the southern end of the Pennines. Mostly in Derbyshire, it extends into Cheshire, Greater Manchester, Staffordshire, West Yorkshire and South Yorkshire. It is subdivided into the Dark Peak, moorland dominated by gritstone, and the White Peak, a limestone area with valleys and gorges. The Dark Peak forms an arc on the north, east and west of the district, and the White Peak covers central and southern areas. The highest point is Kinder Scout (). Most of the area is within the Peak District National Park, a protected landscape designated in 1951. A 2021 report states that "the Park's own population numbers around 40,000 and supports an estimated 18,000 jobs, predominantly through farming, manufacturing and, inevitably, tourism". The area has been inhabited since the Mesolithic era; it was largely used for agricultural purposes until mining arose in the Middle Ages. During the Industrial Revolution, seve ...
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South Pennines
The South Pennines is a region of moorland and hill country in northern England lying towards the southern end of the Pennines. In the west it includes the Rossendale Valley and the West Pennine Moors. It is bounded by the Greater Manchester conurbation in the west and the Bowland Fells and Yorkshire Dales to the north. To the east it is fringed by the towns of West Yorkshire whilst to the south it is bounded by the Peak District. The rural South Pennine Moors constitutes both a Site of Special Scientific Interest and Special Area of Conservation. National character area The Southern Pennines National Character Area defined by Natural England includes the West Pennine Moors and is a landscape of broad moorland, flat-topped hills and fields enclosed by dry stone walls. Settlements built from local gritstone occupy river valleys with wooded sides. Peat soils and blanket bog on the moors store carbon while high rainfall fills many reservoirs supplying water to the adjacent conurb ...
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