|
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Mersey
The River Mersey () is a major river in North West England. Its name derives from Old English and means "boundary river", possibly referring to its having been a border between the ancient kingdoms of Mercia and Northumbria. For centuries it has formed part of the boundary between the historic counties of Lancashire and Cheshire. The Mersey starts at the confluence of the River Tame and River Goyt in Stockport. It flows westwards through south Manchester, then into the Manchester Ship Canal near Irlam Locks, becoming a part of the canal and maintaining its water levels. After it exits the canal, flowing towards Warrington where it widens. It then narrows as it passes between Runcorn and Widnes. The river widens into a large estuary, which is across at its widest point near Ellesmere Port. The course of the river then turns northwards as the estuary narrows between Liverpool and Birkenhead on the Wirral Peninsula to the west, and empties into Liverpool Bay. In total the ... [...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 parishes in England, civil parish of the Metropolitan Borough of Oldham in Greater Manchester, England. It comprises several villages and Hamlet (place), hamlets as well as suburbs of Oldham on the Saddleworth Moor, west side of the Pennines, Pennine hills. Areas include Austerlands, Delph, Denshaw, Diggle, Greater Manchester, Diggle, Dobcross, Friezland, Grasscroft, Greenfield, Greater Manchester, Greenfield, Grotton, Lydgate, Greater Manchester, Lydgate, Scouthead, Springhead, Greater Manchester, 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. Historic counties of England, 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 (textiles), spinning and weaving. By the en ... [...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 A county () is a geographic region of a country used for administrative or other purposesL. Brookes (ed.) '' Chambers Dictionary''. Edinburgh: Chambers Harrap Publishers Ltd, 2005. in some nations. The term is derived from the Old French denoti ... Highest point English counties ... [...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 ... [...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 at Springwater Park, located 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 compoun ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Medlock
The River Medlock in Greater Manchester, England rises in east 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 eastern side of Oldham MBC, 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 Stre ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Irk
The River Irk is a river in the historic county of Lancashire in North West England that flows through the northern part of Greater Manchester. It rises to the east of Royton and runs west past Chadderton, Middleton and Blackley before merging with the River Irwell, a tributary of the River Mersey, 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, the bu ... [...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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Etherow
The River Etherow in northern England is 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 Marple. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Douglas, Lancashire
The River Douglas, also known as the River Asland or Astland, flows through parts of Lancashire and Greater Manchester in North West England. It is a tributary of the River Ribble and has several tributaries, the major ones being the River Tawd and the River Yarrow. In 1720, an act of Parliament, the ( 6 Geo. 1. c. 28), authorized Thomas Steers and William Squire to make the River Douglas navigable to small ships between Wigan and its mouth. Despite financial irregularities, the Douglas Navigation was not completed until 1742. By 1783, it had been replaced by the Leeds and Liverpool Canal, and the river reverted to its natural state. Although the remnants of several locks are still visible between Parbold and Gathurst. The Rufford Branch of the canal joins the river at Tarleton. The river rises on Winter Hill in the West Pennine Moors, and flows for through several towns before reaching the Ribble estuary near Tarleton, with the last being tidal. In 1892, the Douglas ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
