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The Valley

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A valley is an elongated low area often running between hills or mountains and typically containing a river or stream running from one end to the other. Most valleys are formed by erosion of the land surface by rivers or streams over a very long period. Some valleys are formed through erosion by glacial ice . These glaciers may remain present in valleys in high mountains or polar areas.

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57-539: The Valley or The Valleys may refer to: Places known as "The Valley" [ edit ] The Valley (stadium) , home ground of Charlton Athletic Football Club The Valley, Anguilla , the capital of Anguilla The Valleys or the South Wales Valleys , United Kingdom Moonee Valley Racecourse , a horse racing track in Melbourne, Australia Tóin an tSeanbhaile ,

114-615: A lease for the club to use the stadium until January 2035. On 24 September 2022, the Valley hosted a charity match, in which the YouTube group Sidemen played against other major YouTube personalities who formed the YouTube All-Stars, which included Darren Watkins , also known as IShowSpeed. Mark Clattenburg was the match referee. The match, the Sidemen's third one at the Valley, ended 8-7 for

171-468: A 1976 amateur film by Peter Jackson The Valley (2014 film) , a 2014 Lebanese film The Valley (2017 film) , an American drama film La Vallée (film) , a 1972 French film also known as The Valley The Valley , a fictional television series on The O.C. The Valleys (TV series) , a British reality series The Valley (TV series) , a 2024 American reality television series Literature [ edit ] The Valley (novel) ,

228-400: A 2005 novel by Barry Pilton The Valley , the final chapter of The Western Lands Music [ edit ] The Valley (band) , a band from Sydney The Valley (Ashton Nyte album) (2009) The Valley (Betty Who album) (2017) The Valley (Whitechapel album) (2019) The Valley , a 2011 Eisley album "The Valley", a 2016 single by Clare Maguire "The Valley",

285-414: A broader floodplain may result. Deposition dominates over erosion. A typical river basin or drainage basin will incorporate each of these different types of valleys. Some sections of a stream or river valleys may have vertically incised their course to such an extent that the valley they occupy is best described as a gorge , ravine , or canyon . Rapid down-cutting may result from localized uplift of

342-527: A cirque glacier. During glacial periods, for example, the Pleistocene ice ages, it is in these locations that glaciers initially form and then, as the ice age proceeds, extend downhill through valleys that have previously been shaped by water rather than ice. Abrasion by rock material embedded within the moving glacial ice causes the widening and deepening of the valley to produce the characteristic U or trough shape with relatively steep, even vertical sides and

399-584: A narrow valley with steep sides. Gill is used to describe a ravine containing a mountain stream in Cumbria and the Pennines . The term combe (also encountered as coombe ) is widespread in southern England and describes a short valley set into a hillside. Other terms for small valleys such as hope, dean, slade, slack and bottom are commonly encountered in place-names in various parts of England but are no longer in general use as synonyms for valley . The term vale

456-432: A relatively flat bottom. Interlocking spurs associated with the development of river valleys are preferentially eroded to produce truncated spurs , typical of glaciated mountain landscapes. The upper end of the trough below the ice-contributing cirques may be a trough-end . Valley steps (or 'rock steps') can result from differing erosion rates due to both the nature of the bedrock (hardness and jointing for example) and

513-465: A slower rate than that of the main valley floor; thus the difference in the two valleys' depth increases over time. The tributary valley, composed of more resistant rock, then hangs over the main valley. Trough-shaped valleys also form in regions of heavy topographic denudation . By contrast with glacial U-shaped valleys, there is less downward and sideways erosion. The severe downslope denudation results in gently sloping valley sides; their transition to

570-597: A song from Duran Duran's album Red Carpet Massacre "The Valley", a song by The Interrupters from the 2016 album Say it out Loud "The Valley", a song from Jane Siberry's album Bound by the Beauty "The Valley", a song by Keshia Chanté "The Valley", a song by Los Lobos on The Town and the City (album) (2006) "The Valley", a song by the Oh Hellos "The Valleys", a song from The Mountains ' album The Mountains,

627-523: A supporting pillar. The Valley's highest average attendance came in the 1948–49 season when crowds averaged 40,216, making Charlton one of only thirteen clubs in English football to achieve a seasonal average of 40,000+. The Valley's lowest average attendance is 5,108 from the 1984–85 season. Highest Division One Lowest Division Two Division Three Division Three South Division Two Average attendance for every season since 1993–94,

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684-427: A valley between its sides is referred to as the valley floor. The valley floor is typically formed by river sediments and may have fluvial terraces . The development of a river valley is affected by the character of the bedrock over which the river or stream flows, the elevational difference between its top and bottom, and indeed the climate. Typically the flow will increase downstream and the gradient will decrease. In

741-500: A variety of transitional forms between V-, U- and plain valleys can form. The floor or bottom of these valleys can be broad or narrow, but all valleys have a shoulder. The broader a mountain valley, the lower its shoulders are located in most cases. An important exception is canyons where the shoulder almost is near the top of the valley's slope. In the Alps – e.g. the Tyrolean Inn valley –

798-454: A village on Achill Island, Co. Mayo, Ireland, known colloquially in English as The Valley San Fernando Valley , California Phoenix metropolitan area , Arizona Lower Rio Grande Valley , Texas Lower Naugatuck Valley , Connecticut Artworks [ edit ] The Valley (suite) , a 1990 suite of etchings by Keith Haring with text by William S. Burroughs Film and television [ edit ] The Valley (1976 film) ,

855-670: A watercourse only rarely. In areas of limestone bedrock , dry valleys may also result from drainage now taking place underground rather than at the surface. Rift valleys arise principally from earth movements , rather than erosion. Many different types of valleys are described by geographers, using terms that may be global in use or else applied only locally. Valleys may arise through several different processes. Most commonly, they arise from erosion over long periods by moving water and are known as river valleys. Typically small valleys containing streams feed into larger valleys which in turn feed into larger valleys again, eventually reaching

912-405: Is a tributary valley that is higher than the main valley. They are most commonly associated with U-shaped valleys, where a tributary glacier flows into a glacier of larger volume. The main glacier erodes a deep U-shaped valley with nearly vertical sides, while the tributary glacier, with a smaller volume of ice, makes a shallower U-shaped valley. Since the surfaces of the glaciers were originally at

969-559: Is a sports stadium in Charlton, London , England with a capacity of 27,111, which has been the home of Charlton Athletic Football Club since the 1920s, with a period of exile between 1985 and 1992. The stadium is served by Charlton railway station , which is less than a five-minute walk away from the stadium. An alternative is to use the Jubilee line , exiting at North Greenwich, and changing for route 161, 472 and 486 buses, which stop outside

1026-465: Is high. On 9 April 2021, the club announced that from the start of 2021–22 season, the stand would be renamed to the Alan Curbishley Stand in honour of the former player and manager, and to celebrate the 30th anniversary of when Curbishley was appointed manager of the club - a role he held from 1991 to 2006. Capacity: 8,097 The West Stand was built in 1998 after Charlton's first promotion to

1083-501: Is only 50 meters (160 ft) deep while the main fjord is around 1,300 meters (4,300 ft) at the same point. Glaciated terrain is not the only site of hanging streams and valleys. Hanging valleys are also simply the product of varying rates of erosion of the main valley and the tributary valleys. The varying rates of erosion are associated with the composition of the adjacent rocks in the different valley locations. The tributary valleys are eroded and deepened by glaciers or erosion at

1140-481: Is the word cwm borrowed from Welsh . The word dale occurs widely in place names in the north of England and, to a lesser extent, in southern Scotland. As a generic name for a type of valley, the term typically refers to a wide valley, though there are many much smaller stream valleys within the Yorkshire Dales which are named "(specific name) Dale". Clough is a word in common use in northern England for

1197-614: Is used in England and Wales to describe a wide river valley, usually with a particularly wide flood plain or flat valley bottom. In Southern England, vales commonly occur between the outcrops of different relatively erosion-resistant rock formations, where less resistant rock, often claystone has been eroded. An example is the Vale of White Horse in Oxfordshire. Some of the first human complex societies originated in river valleys, such as that of

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1254-496: The Nile , Tigris-Euphrates , Indus , Ganges , Yangtze , Yellow River , Mississippi , and arguably the Amazon . In prehistory , the rivers were used as a source of fresh water and food (fish and game), as well as a place to wash and a sewer. The proximity of water moderated temperature extremes and provided a source for irrigation , stimulating the development of agriculture . Most of

1311-664: The first civilizations developed from these river valley communities. Siting of settlements within valleys is influenced by many factors, including the need to avoid flooding and the location of river crossing points. Numerous elongate depressions have been identified on the surface of Mars , Venus , the Moon , and other planets and their satellites and are known as valles (singular: 'vallis'). Deeper valleys with steeper sides (akin to canyons) on certain of these bodies are known as chasmata (singular: 'chasma'). Long narrow depressions are referred to as fossae (singular: 'fossa'). These are

1368-519: The Covered End Upper ahead of Charlton's 2024-25 season , it will have a capacity of 1,064. The club has also received provisional permission to install a safe standing area in the Covered End Lower. Capacity: 5,802 The East Stand was constructed during the 1993–94 season and fully completed in 1994. As part of the first development to the ground since the return in 1992, it replaced

1425-501: The Premier League and is also two tiered. This is the main stand at the Valley with the largest capacity, and also houses the club's offices, as well as the director's box, board room dug-outs, changing rooms and the commercial centre (ticket office). There are also many conferencing rooms in this stand which are used for official and community events. There is a large statue of Sam Bartram , (considered to be Charlton's finest player) at

1482-513: The Scandinavian ice sheet during the various ice ages advanced slightly uphill against the lie of the land. As a result, its meltwaters flowed parallel to the ice margin to reach the North Sea basin, forming huge, flat valleys known as Urstromtäler . Unlike the other forms of glacial valleys, these were formed by glacial meltwaters. Depending on the topography , the rock types , and the climate ,

1539-624: The Sidemen and raised over £1,000,000 split between the Teenage Cancer Trust , CALM , Rays of Sunshine and M7 Education charities. In March 2024, Charlton announced their intention to build a safe standing area which would be completed over the summer. Additional to this, the club had worked worked alongside the Charlton Athletic Supporters Trust to implement one of the UK's first 'Youth Specific Sections' for fans. In 2024, it

1596-511: The Valleys, the Lakes (2014) Schools [ edit ] The Valley School , Bangalore, India The Valley Secondary School , former name of Albena Lake-Hodge Comprehensive School, Anguilla See also [ edit ] Valley , a geographical feature Valley (disambiguation) Topics referred to by the same term [REDACTED] This disambiguation page lists articles associated with

1653-504: The actual valley bottom is unclear. Trough-shaped valleys occur mainly in periglacial regions and in tropical regions of variable wetness. Both climates are dominated by heavy denudation. Box valleys have wide, relatively level floors and steep sides. They are common in periglacial areas and occur in mid-latitudes, but also occur in tropical and arid regions. Rift valleys, such as the Albertine Rift and Gregory Rift are formed by

1710-472: The adjoining earthworks. The unique circumstances of the ground's initial construction led to an unusually intense bond between the club's supporters and the site that still exists. In the 1923–24 season, Charlton played at The Mount stadium in Catford but in a much more highly populated area. A proposed merger with Catford South End FC fell through and so Charlton moved back to the Valley. In 1967, Len Silver

1767-426: The club's debts led to it almost going out of business. A consortium of supporters successfully acquired the club in 1984, but the Valley remained in the possession of the ownership of the former owner, and the club was unable to finance the improvements needed to meet new safety requirements. Shortly after the start of the 1985–86 season, Charlton left the Valley, entering into an agreement with Crystal Palace to share

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1824-500: The entrance of the West Stand. Capacity: 3,469 The Jimmy Seed (or South) Stand is the oldest part of the ground, and dates from the early 1980s. This stand is named after Charlton's manager, Jimmy Seed (1895–1966) – with whom Charlton won the FA Cup in 1947. This stand has a capacity of around 3,000 and hosts the away supporters at games. It is also the only part of the Valley with

1881-599: The expansion of the Earth 's crust due to tectonic activity beneath the Earth's surface. There are many terms used for different sorts of valleys. They include: Similar geographical features such as gullies , chines , and kloofs , are not usually referred to as valleys. The terms corrie , glen , and strath are all Anglicisations of Gaelic terms and are commonly encountered in place-names in Scotland and other areas where Gaelic

1938-643: The first full season since Charlton returned to the Valley. First Division Premier League Championship League One *Last 5 home matches played behind close doors due to the COVID-19 pandemic . **Due to the COVID-19 pandemic all home matches were played behind closed doors except for two matches which had limited crowds. Valley At lower latitudes and altitudes, these glacially formed valleys may have been created or enlarged during ice ages but now are ice-free and occupied by streams or rivers. In desert areas, valleys may be entirely dry or carry

1995-443: The flow slower and both erosion and deposition may take place. More lateral erosion takes place in the middle section of a river's course, as strong currents on the outside of its curve erode the bank. Conversely, deposition may take place on the inside of curves where the current is much slacker, the process leading to the river assuming a meandering character. In the lower valley, gradients are lowest, meanders may be much broader and

2052-516: The ground's capacity to over 40,000 by expanding the east side and completely rebuilding the south side, but these plans were abandoned after Charlton were relegated from the Premier League in 2007. In 2004, the Unity Cup was held at the Valley, with Nigeria winning the competition. Charlton's former owner Roland Duchâtelet retained ownership of The Valley after selling the football club in 2020, but subsequent owner, Thomas Sandgaard , negotiated

2109-427: The land surface or rejuvenation of the watercourse as a result for example of a reduction in the base level to which the river is eroded, e.g. lowered global sea level during an ice age . Such rejuvenation may also result in the production of river terraces . There are various forms of valleys associated with glaciation. True glacial valleys are those that have been cut by a glacier which may or may not still occupy

2166-610: The large terraces were no longer seen as desirable or safe. Charlton Athletic supporters proposed to completely rebuild the stadium so that the club could return there at the beginning of the 1990s. However, the Greenwich Borough Council overwhelmingly turned down the plans to renovate the ground. Club supporters formed their own local political party, the Valley Party, in response to the council's decision. The party ran candidates for all but two Greenwich Council seats, sparing

2223-481: The latter's Selhurst Park facilities, the first official groundsharing arrangement in the Football League in 36 years. In 1988, the ownership of the club and the Valley were again united and, in a "grass roots" effort that harked back to the ground's initial construction, thousands of supporters volunteered to clean the venue, eventually burning the debris in a huge bonfire on the pitch. By that time, however,

2280-507: The massive east terrace, which had remained closed and prohibited from use since the mid-1980s after the Bradford City stadium fire . The East Stand consists of a single tier of seats and houses the television gantry, and also has numerous executive boxes. Occasionally, for FA and League Cup matches, part of the East Stand is used to house away supporters if the demand for away team tickets

2337-463: The ocean or perhaps an internal drainage basin . In polar areas and at high altitudes, valleys may be eroded by glaciers ; these typically have a U-shaped profile in cross-section, in contrast to river valleys, which tend to have a V-shaped profile. Other valleys may arise principally through tectonic processes such as rifting . All three processes can contribute to the development of a valley over geological time. The flat (or relatively flat) portion of

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2394-436: The power of the moving ice. In places, a rock basin may be excavated which may later be filled with water to form a ribbon lake or else by sediments. Such features are found in coastal areas as fjords . The shape of the valley which results from all of these influences may only become visible upon the recession of the glacier that forms it. A river or stream may remain in the valley; if it is smaller than one would expect given

2451-493: The promoter at Hackney made an application to open Charlton as a British League speedway club, and plans were proposed to construct a track around the perimeter of the football pitch. The application was enthusiastically supported initially, but was eventually ruled out on the grounds of noise nuisance. For many years, the Valley was one of the largest Football League grounds in Britain, although its highest maximum capacity of 75,000

2508-534: The re-opening faced a series of delays before finally occurring in December 1992. Since then, the ground has undergone some remarkable changes. The north, east and west sides have almost been completely rebuilt, which gave the ground a capacity of over 27,000 by December 2001, when Charlton were in the second season of a stay in the FA Premier League which would last for seven seasons. The club had ambitions to extend

2565-446: The same elevation , the shallower valley appears to be 'hanging' above the main valley. Often, waterfalls form at or near the outlet of the upper valley. Hanging valleys also occur in fjord systems underwater. The branches of Sognefjord are much shallower than the main fjord. The mouth of Fjærlandsfjord is about 400 meters (1,300 ft) deep while the main fjord nearby is 1,200 meters (3,900 ft) deep. The mouth of Ikjefjord

2622-543: The shoulders are quite low (100–200 meters above the bottom). Many villages are located here (esp. on the sunny side) because the climate is very mild: even in winter when the valley's floor is filled with fog, these villages are in sunshine . In some stress-tectonic regions of the Rocky Mountains or the Alps (e.g. Salzburg ), the side valleys are parallel to each other, and are hanging . Smaller streams flow into rivers as deep canyons or waterfalls . A hanging valley

2679-427: The site. An army of volunteer Charlton supporters dug out a flat area for the pitch at the bottom of the chalk pit and used the excavated material to build up makeshift stands. The ground's name most likely comes from its original valley-like appearance. The club played its first game at the ground before any seats, or even terraces, were installed. There was simply a roped-off pitch with the crowd standing or sitting on

2736-849: The size of its valley, it can be considered an example of a misfit stream . Other interesting glacially carved valleys include: A tunnel valley is a large, long, U-shaped valley originally cut under the glacial ice near the margin of continental ice sheets such as that now covering Antarctica and formerly covering portions of all continents during past glacial ages. Such valleys can be up to 100 km (62 mi) long, 4 km (2.5 mi) wide, and 400 m (1,300 ft) deep (its depth may vary along its length). Tunnel valleys were formed by subglacial water erosion . They once served as subglacial drainage pathways carrying large volumes of meltwater. Their cross-sections exhibit steep-sided flanks similar to fjord walls, and their flat bottoms are typical of subglacial glacial erosion. In northern Central Europe,

2793-484: The stadium. In Charlton's early years, the club had a nomadic existence, using several different grounds between its formation in 1905 and the beginning of World War I in 1914. The Valley dates from 1919, at a time when Charlton were moderately successful and looking for a new home. Fred Barned, the club’s honorary chairman, found an abandoned sand and chalk pit in Charlton, but did not have sufficient funds to fully develop

2850-471: The title The Valley . If an internal link led you here, you may wish to change the link to point directly to the intended article. Retrieved from " https://en.wikipedia.org/w/index.php?title=The_Valley&oldid=1259502191 " Category : Disambiguation pages Hidden categories: Short description is different from Wikidata All article disambiguation pages All disambiguation pages The Valley (stadium) The Valley

2907-416: The two councillors who had approved the new stadium plans. The party won almost 15,000 votes in the 1990 local elections, successfully pressuring the council to approve the plans for the new stadium. In 1991, construction began on the new Valley, and the club moved from Selhurst Park to West Ham's Upton Park . It was originally hoped that the club would return to the stadium before Christmas that year, but

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2964-407: The upper valley, the stream will most effectively erode its bed through corrasion to produce a steep-sided V-shaped valley. The presence of more resistant rock bands, of geological faults , fractures , and folds may determine the course of the stream and result in a twisting course with interlocking spurs . In the middle valley, as numerous streams have coalesced, the valley is typically wider,

3021-407: The valley at the present day. Such valleys may also be known as glacial troughs. They typically have a U-shaped cross-section and are characteristic landforms of mountain areas where glaciation has occurred or continues to take place. The uppermost part of a glacial valley frequently consists of one or more 'armchair-shaped' hollows, or ' cirques ', excavated by the rotational movement downslope of

3078-537: Was also announced a new hybrid pitch would be installed as part of a six-figure investment by the club's owners, and a £750,000 grant from the Premier League Stadium Fund. As part of the investment, the Charlton women's team would play all of their home matches at The Valley for the first time. Their first match at The Valley took place on 28 April 2024, ending in a 2–0 victory against Southampton in front of 985 fans. Capacity: 9,743 The North Stand

3135-445: Was built as a replacement for the 'covered end', and is still called by this name. It was built during the 2001–02 season as part of the developments to bring the Valley's capacity to 26,500 after promotion to the Premier League in 2000. The North Stand houses the most vocal supporters in the ground in particular the upper tier alongside a drum, along with restaurants and executive suites. A safe standing area will be installed in

3192-414: Was once widespread. Strath signifies a wide valley between hills, the floor of which is either level or slopes gently. A glen is a river valley which is steeper and narrower than a strath. A corrie is a basin-shaped hollow in a mountain. Each of these terms also occurs in parts of the world formerly colonized by Britain . Corrie is used more widely by geographers as a synonym for (glacial) cirque , as

3249-524: Was only half the capacity of Glasgow's Hampden Park . However, Charlton's long absence from the top level of English football prevented much-needed renovation, because funds dried up and attendances fell. Charlton were relegated from the First Division in 1957 and did not return until 1986. In 1972, the club was relegated to the Third Division for the first time in the post-war era. In the early 1980s,

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