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Geography Of Greater Manchester
The geography of Greater Manchester is dominated by one of the United Kingdom's largest metropolitan areas, and in this capacity the landlocked metropolitan county constitutes one of the most urbanised and densely populated areas of the country. There is a mix of high density urban areas, suburbs, semi-rural and rural locations in Greater Manchester, but overwhelmingly the land use in the county is urban. Greater Manchester is a landlocked county spanning ( 39th largest in England). The Pennines rise along the eastern side of the county, through parts of the boroughs of Oldham, Rochdale and Tameside. The West Pennine Moors, as well as a number of coalfields (mainly sandstones and shales) lie in the west of the county. The rivers Mersey, Irwell and Tame run through the county boundaries, each of which rise in the Pennines. Other rivers run through the county, including the Beal, the Douglas, the Etherow, the Goyt, the Irk, the Medlock and the Roch. Black Chew Head is the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Manchester From Billinge Hill
Manchester () is a city in Greater Manchester, England. It had a population of 552,000 in 2021. It is bordered by the Cheshire Plain to the south, the Pennines to the north and east, and the neighbouring city of Salford to the west. The two cities and the surrounding towns form one of the United Kingdom's most populous conurbations, the Greater Manchester Built-up Area, which has a population of 2.87 million. The history of Manchester began with the civilian settlement associated with the Roman fort ('' castra'') of ''Mamucium'' or ''Mancunium'', established in about AD 79 on a sandstone bluff near the confluence of the rivers Medlock and Irwell. Historically part of Lancashire, areas of Cheshire south of the River Mersey were incorporated into Manchester in the 20th century, including Wythenshawe in 1931. Throughout the Middle Ages Manchester remained a manorial township, but began to expand "at an astonishing rate" around the turn of the 19th century. Manchester's u ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Irwell
The River Irwell ( ) is a tributary of the River Mersey in north west England. It rises at Irwell Springs on Deerplay Moor, approximately north of Bacup and flows southwards for to meet the Mersey near Irlam. The Irwell marks the boundary between Manchester and Salford, and its lower reaches have been canalised and now form part of the Manchester Ship Canal. In the 17th and 18th centuries, the Irwell's lower reaches were a trading route that became part of the Mersey and Irwell Navigation. In the 19th century, the river's course downstream of Manchester was permanently altered by the construction of the Manchester Ship Canal which opened in 1896. The canal turned Manchester and Salford into a major inland seaport and led to the development of Trafford Park which became the largest industrial estate in Europe. Further changes were made in the 20th and 21st centuries to prevent flooding in Manchester and Salford, including the construction of the Anaconda Cut in 1970 and the Ri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wardle, Greater Manchester
Wardle (; pop. 7,092) is a village near Littleborough within the Metropolitan Borough of Rochdale, in Greater Manchester, England. It lies amongst the foothills of the South Pennines, east-southeast of Whitworth, north-northwest of Rochdale and north-northeast of the city of Manchester. Historically a part of Lancashire, Wardle and its surroundings have provided archaeological evidence of Mesolithic activity in the area. The name Wardle is said to be derived from "Ward Hill", implying "fortified place". Brown Wardle Hill overlooks the village from the north, its name being derived from the Celtic word ''bron'' meaning "round". During the Middle Ages Wardle was a small centre of domestic flannel and woollen cloth production, and many of the original weavers' cottages survive today as listed buildings. Wardle, the most northerly settlement in Greater Manchester,Rochdale Metropolitan Borough Council (N.D.), p. 33. encompasses small parts of Smallbridge and Dearnley â ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chat Moss
Chat Moss is a large area of peat bog that makes up part of the City of Salford, Metropolitan Borough of Wigan and Trafford in Greater Manchester, England. It also makes up part of Metropolitan Borough of St Helens in Merseyside and Warrington in Cheshire. North of the Manchester Ship Canal and River Mersey, to the west of Manchester, it occupies an area of about . As it might be recognised today, Chat Moss is thought to be about 7,000 years old, but peat development seems to have begun there with the ending of the last ice age, about 10,000 years ago. The depth of peat ranges from . A great deal of reclamation work has been carried out, particularly during the 19th century, but a large-scale network of drainage channels is still required to keep the land from reverting to bog. In 1958 workers extracting peat discovered the severed head of what is believed to be a Romano-British Celt, possibly a sacrificial victim, in the eastern part of the bog near Worsley. Much of Ch ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saddleworth
Saddleworth is a civil parish of the Metropolitan Borough of Oldham in Greater Manchester, England. It comprises several villages and hamlets as well as suburbs of Oldham on the west side of the Pennine hills. Areas include Austerlands, Delph, Denshaw, Diggle, Dobcross, Friezland, Grasscroft, Greenfield, Grotton, Lydgate, Scouthead, Springhead and Uppermill. Saddleworth lies east of Oldham and northeast of Manchester. It is broadly rural and had a population of 25,460 at the 2011 Census, making it one of the larger civil parishes in the United Kingdom. Historically in the West Riding of Yorkshire and following the Industrial Revolution, in the 18th and 19th centuries, Saddleworth became a centre for cotton spinning and weaving. By the end of Queen Victoria's reign, mechanised textile production had become a vital part of the local economy. The Royal George Mill, owned by the Whitehead family, manufactured felt used for pianofortes, billiard tables and flags. Following th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of English Counties By Highest Point
This is a list of the ceremonial counties of England by their highest point. See also *List of counties of England and Wales in 1964 by highest point *List of mountains and hills of the United Kingdom *List of Scottish council areas by highest point * List of Scottish counties by highest point *List of Welsh principal areas by highest point * List of Northern Ireland districts by highest point *List of Northern Ireland counties by highest point References SourcesCounty and Unitary Authority Topsfrom the ''Database of British and Irish Hills'', which holds information on all English county and unitary authority tops. {{Mountains of Great Britain and Ireland Counties Highest point English counties The counties of England are areas used for different purposes, which include administrative, geographical, cultural and political demarcation. The term "county" is defined in several ways and can apply to similar or the same areas used by each ... ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Black Chew Head
Black Chew Head in Saddleworth in the Metropolitan Borough of Oldham is the highest point or county top of Greater Manchester in northern England. It stands on moorland on the edge of the Peak District at a height of above sea level, close to the border with the High Peak district of Derbyshire. Historically in the West Riding of Yorkshire (along with the rest of Saddleworth), it became a county top in 1974 on the creation of Greater Manchester following the Local Government Act 1972. Location and access Black Chew Head is an outlying part of Black Hill, meaning Kinder Scout is its parent peak. It overlooks the Chew Valley, which leads eastwards and northwards to Dovestones Reservoir, and the valley of Crowden Great Brook leading south to Longdendale. The hill is accessible by many routes: the most used and most obvious is from Dovestones Reservoir in Greenfield via the Chew Reservoir access road. The hill is also accessible from Crowden in Derbyshire and from the A635 t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Roch
The River Roch is a river in Greater Manchester in North West England, a tributary of the River Irwell. Course Rising on Chelburn Moor (south of Todmorden in the Pennines), the river flows south through Littleborough towards Rochdale where it is joined by the River Beal at Belfield, and the River Spodden from Whitworth. Turning west it runs past Heywood and Bury before meeting the River Irwell just to the east of Radcliffe. Etymology The town of Rochdale is recorded as ''Recedham'' in the Domesday Book and ''Rachetham'' in 1193, with variations of ''Rechedham'' continuing into the thirteenth century.Mills, A.D.: ''A Dictionary of English Place Names'', 2nd Edition, page 289, s.n. Rochdale. Oxford University Press, 1998 It is thought that these names represent a pre-existing Brittonic name for the river Roch, borrowed into Old English for the name of the settlement. The early forms of ''Rachet-ham'' and ''Reched-ham'' suggest a compound of two elements, ''ro-ced'' or '' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Medlock
The River Medlock is a river in Greater Manchester, England, which rises near Oldham and flows south and west for to join the River Irwell in Manchester city centre. Sources Rising in the hills that surround Strinesdale just to the east of Oldham, the Medlock flows through the steep-sided wooded gorge that separates Lees from Ashton-under-Lyne and the Daisy Nook Country Park with its 19th century aqueduct carrying the disused Hollinwood Branch Canal over the shallow river. Lower reaches The final miles of the river flowing to the River Irwell have been extensively modified. The river is culverted underneath the car park of the City of Manchester Stadium (the site of a former gasworks). It is visible flowing through Mayfield Park and under a bridge on Baring Street, close to Piccadilly station, before running again in a culvert beneath the former University of Manchester Institute of Science & Technology campus (London Road (A6) to Princess Street), then under Hulme St ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Irk
The River Irk is a river in the historic county of Lancashire in the North West England that flows through the northern most Lancastrian towns of the ceremonial county of Greater Manchester. It rises to the east of Royton and runs west past Chadderton, Middleton and Blackley before merging with the River Irwell in the centre of Manchester. History The Irk's name is of obscure etymology, but may be Brittonic in origin and related to the Welsh word ''iwrch'', meaning roebuck. The Afon Iwrch, a river in Denbighshire, also takes its name from this word. In medieval times, there was a mill by the Irk at which the tenants of the manor ground their corn and its fisheries were controlled by the lord of the manor. In the 16th century, throwing carrion and other offensive matter into the Irk was forbidden. Water for Manchester was drawn from the river before the Industrial Revolution. A bridge over the Irk was recorded in 1381. The river was noted for destructive floods. In 1480 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Goyt
The River Goyt is a tributary of the River Mersey in North West England. Etymology The name ''Goyt'' may be derived from the Middle English ''gote'', meaning "a watercourse, a stream". Derivation from the Welsh ''gwyth'' meaning "vein" has been suggested, but described as "doubtful". Course The Goyt rises on the moors of Axe Edge, near the River Dane and the Cat and Fiddle Inn. The area is known as the Upper Goyt Valley. The old Cat and Fiddle Road from Buxton to Macclesfield crosses the river just as it turns northwards to flow down its well-known valley. The river then flows under Derbyshire Bridge, which was the old boundary between Derbyshire and Cheshire. Later it reaches an old packhorse bridge that was moved when Errwood reservoir was built in the 1960s (see photo below). Further downstream there is another reservoir, the Fernilee Reservoir, built in 1938. The original line of the Cromford and High Peak Railway can be seen near this point. The Goyt then passes thr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Etherow
The River Etherow is a river in northern England, and a tributary of the River Goyt. Although now passing through South Yorkshire, Derbyshire and Greater Manchester, it historically formed the ancient county boundary between Cheshire and Derbyshire. The upper valley is known as Longdendale. The river has a watershed of approximately , and the area an annual rainfall of . Course Rising in the Redhole Spring and Wike Head area of Pikenaze Moor in Derbyshire, the river broadens into the Longdendale Chain of reservoirs in the Peak District National Park. It emerges again in Tintwistle, Derbyshire, at the foot of Bottoms Reservoir dam and passes Melandra Castle in Gamesley, where it is joined by Glossop Brook.This brook takes in waters from the Shelf Brook, Hurst Brook and others. The Etherow enters the borough of Tameside at Hollingworth in Greater Manchester, passing into Stockport where it passes through Etherow Country Park. It flows into the River Goyt at Brabyns Park near ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
.jpg "Click for more on -> River Medlock")
