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Amersham
Amersham ( ) is a market town and civil parish in Buckinghamshire, England, in the Chiltern Hills, northwest of central London, south-east of Aylesbury and north-east of High Wycombe. Amersham is part of the London commuter belt. There are two distinct areas: * Old Amersham, set in the valley of the River Misbourne, containing the 13th-century parish church of St. Mary's and several old pubs and coaching inns * Amersham-on-the-Hill, which grew in the early 20th century around Amersham station, which was served by the Metropolitan Railway, now the Metropolitan line, and the Great Central Railway. Geography Old Amersham occupies the valley floor of the River Misbourne. This is a chalk stream which dries up periodically. The river occupies a valley much larger than it is possible for a river the size of the present River Misbourne to cut, which makes it a misfit stream. The valley floor is at around OD, and the valley top is at around OD. It is likely that the va ...
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Market Town
A market town is a settlement most common in Europe that obtained by custom or royal charter, in the Middle Ages, a market right, which allowed it to host a regular market; this distinguished it from a village or city. In Britain, small rural towns with a hinterland of villages are still commonly called market towns, as sometimes reflected in their names (e.g. Downham Market, Market Rasen, or Market Drayton). Modern markets are often in special halls, but this is a recent development, and the rise of permanent retail establishments has reduced the need for periodic markets. Historically the markets were open-air, held in what is usually called (regardless of its actual shape) the market square (or "Market Place" etc), and centred on a market cross ( mercat cross in Scotland). They were and are typically open one or two days a week. History The primary purpose of a market town is the provision of goods and services to the surrounding locality. Although market towns were kno ...
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Great Central Railway
The Great Central Railway in England was formed when the Manchester, Sheffield and Lincolnshire Railway changed its name in 1897, anticipating the opening in 1899 of its London Extension. On 1 January 1923, the company was grouped into the London and North Eastern Railway. History New name On assuming its new title, the Great Central Railway had a main line from Manchester London Road Station via , Sheffield Victoria, and Grimsby to . A second line left the line at Penistone and served , and Scunthorpe, before rejoining the Grimsby line at . Other lines linked Sheffield to Barnsley (via ) and Doncaster (via Rotherham) and also and Wrawby Junction. Branch lines in north Lincolnshire ran to Barton-upon-Humber and New Holland and served ironstone quarries in the Scunthorpe area. In the Manchester area, lines ran to Stalybridge and Glossop. In the 1890s, the MS&LR began constructing its Derbyshire lines, the first part of its push southwards. Leaving its east–west mai ...
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Coleshill, Buckinghamshire
Coleshill (formerly Stoke) is a village and civil parish within Chiltern district in Buckinghamshire, England. It is south of Amersham and north of Beaconsfield. History The village name is Anglo Saxon in origin, and means 'Coll's hill', though it has only been known by this name since the early 16th century. It appears as 'Colshull' on John Speed's maps in the early 17th century. Previously it was known as 'Stoke'. In 1844 the village was transferred from Hertfordshire to Buckinghamshire by the Counties (Detached Parts) Act 1844. From 1919 to 1939, the village was home to the Coleshill Convalescent Home, officially opened on 27 June 1919 by Lady Portman. It had 12 beds for soldiers wounded in World War I. Facilities The village has a junior school (Coleshill Church of England Infant School), community hall, two pubs (''The Red Lion'' http://www.theredlioncoleshill.pub and ''The Harte & Magpies''), a tennis club with two courts, and a cricket club. A small play park ex ...
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Seer Green
Seer Green is a village and civil parish in Buckinghamshire, England. It is in the Chiltern Hills, east-north-east of Beaconsfield and south-west of Chalfont St Giles. History The Toponymy, toponym "Seer" is derived from the Norman language, Norman French for "dry or arid place". In Manorialism, manorial rolls of 1223 it was called ''La Sere'', although local legend has it that the "Seer" refers to King Arthur's Court visiting the area and locals consulting his "seer" – a nice story but of doubtful origin. Even so, there is a pub called Merlin's Cave in the nearby village Chalfont St Giles, after this legend. The affix "Green" came later. The Church of England parish church of the Holy Trinity was built in 1846. It is brick and flint with lancet windows. There is also a Baptist Union of Great Britain, Baptist church. Seer Green became a separate parish in 1866, having previously been a hamlet of the parish of Farnham Royal. It had levied a separate poor rate before then. U ...
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Chalfont St Giles
Chalfont St Giles is a village and civil parish in southeast Buckinghamshire, England. It is in a group of villages called The Chalfonts, which also includes Chalfont St Peter and Little Chalfont. It lies on the edge of the Chiltern Hills, west-northwest of Charing Cross, central London, and near Seer Green, Jordans, Chalfont St Peter, Little Chalfont and Amersham. "Chalfont" means chalk spring, in reference to the water-carrying capacities of the local terrain. The cockney rhyming slang term "chalfonts", meaning haemorrhoids (piles), is derived from the name of the village. The village has a duck pond that is fed by the River Misbourne. The village sign was designed and painted by Doreen Wilcockson ARCA in 2001. Chalfont St Giles is famous for the poet Milton's only surviving home. History In the Domesday Book in 1086, Chalfont St Giles and Chalfont St Peter were listed as separate Manors with different owners, called 'Celfunte'. They were separate holdings before the ...
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Little Chalfont
Little Chalfont is a village and civil parish in south-east Buckinghamshire, England. It is one of a group of villages known collectively as The Chalfonts, which also comprises Chalfont St Giles and Chalfont St Peter. Little Chalfont is located around east of Amersham and northwest of Charing Cross, central London. History Little Chalfont is a 20th-century creation triggered by the coming of the Metropolitan Railway. A station called Chalfont Road was opened in 1889 at the northernmost point of Chalfont St Giles Parish where the parishes of Amersham, Chenies, and Chalfont St Giles met. At that time, the area was remote from the centres of the villages and towns, and consisted of isolated farms and cottages, and did not have a specific name. The coming of the railway eventually brought local housing development, and a community developed around the station, which was renamed Chalfont & Latimer station in 1915, a name which it retains today. The first appearance of the name Li ...
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Ley Hill
Ley Hill is a Chiltern village on the Buckinghamshire/ Hertfordshire border in south-east England, near the town of Chesham. It is part of the civil parish of Latimer and Ley Hill, and comes under Chiltern District Council in the County of Buckinghamshire. Ley Hill lies in the Chiltern Hills and is contiguous with Botley. The Common The village has a large common, which is used by Chesham and Ley Hill Golf Club and Ley Hill Cricket Club. Golf has been played on the Common since about 1900. In 2000 a village sign was hung up on the Common which incorporates an owl as the unofficial village emblem. Pubs There are two pubs on the Common called The Swan and The Crown that both serve food. The Swan was built in about 1520, and takes its name from the symbol of the county of Buckinghamshire. In 1680, the timber-framed building consisted of three cottages with five extensions, oak-beamed ceilings and pillars, a kitchen range and an inglenook fireplace. It is reputedly one o ...
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Chesham Bois
Chesham Bois (traditionally , but now more commonly ) is a village in the Chiltern Hills, in Buckinghamshire, England, adjacent to both Amersham and Chesham. History Initially a hamlet in the parish of Chesham, the manor was assessed at 1½ hides in the reign of King Edward the Confessor. The estate belonged to a brother of King Harold, who was killed with him at the Battle of Hastings, and William the Conqueror probably gave this "royal" land to his own half-brother, Odo, Bishop of Bayeux. The village gets its name from the de Bosco family (the French version of which was "de Bois") and by 1213 in the reign of King John a William du Bois was holding the manor. By about 1430, in the reign of Henry VI, the manor had been acquired by the Cheynes of Chenies who remained for over 300 years, before conveying the manor to the Duke of Bedford in 1735. Chesham Bois House, the site of the manor, was the subject of an archaeological excavation by television programme ''Time Team'', ...
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River Chess
The River Chess is a chalk stream that rises near Chesham in the Chiltern Hills, and flows for through Buckinghamshire and Hertfordshire to its confluence with the River Colne, Hertfordshire, River Colne in Rickmansworth. The Chess, along with the River Colne, Hertfordshire, Colne and River Gade, Gade, gives rise to the name of the district of Three Rivers (district), Three Rivers. Etymology The name arose by back-formation from the town of Chesham Chesham (, , or ) is a market town and civil parish in Buckinghamshire, England, south-east of the county town of Aylesbury, north-west of central London, and part of the London commuter belt. It is in the Chess Valley, surrounded by farmla .... It was once known as the Pittlesburne which incorporates the old word ''burn (landform), burna'', used in the Chilterns to describe a clear spring-fed stream on a lower dip-slope, often with a stony bed. Examples are the rivers Misbourne and Bulbourn. River course The River ...
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Water Divide
A drainage divide, water divide, ridgeline, watershed, water parting or height of land is elevated terrain that separates neighboring drainage basins. On rugged land, the divide lies along topographical ridges, and may be in the form of a single range of hills or mountains, known as a dividing range. On flat terrain, especially where the ground is marshy, the divide may be difficult to discern. A triple divide is a point, often a summit, where three drainage basins meet. A ''valley floor divide'' is a low drainage divide that runs across a valley, sometimes created by deposition or stream capture. Major divides separating rivers that drain to different seas or oceans are continental divides. The term ''height of land'' is used in Canada and the United States to refer to a drainage divide. It is frequently used in border descriptions, which are set according to the "doctrine of natural boundaries". In glaciated areas it often refers to a low point on a divide where it is p ...
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Plateau
In geology and physical geography, a plateau (; ; ), also called a high plain or a tableland, is an area of a highland consisting of flat terrain that is raised sharply above the surrounding area on at least one side. Often one or more sides have deep hills or escarpments. Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, and erosion by water and glaciers. Plateaus are classified according to their surrounding environment as intermontane, piedmont, or continental. A few plateaus may have a small flat top while others have wide ones. Formation Plateaus can be formed by a number of processes, including upwelling of volcanic magma, extrusion of lava, Plate tectonics movements and erosion by water and glaciers. Volcanic Volcanic plateaus are produced by volcanic activity. The Columbia Plateau in the north-western United States is an example. They may be formed by upwelling of volcanic magma or extrusion of lava. The un ...
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Dry Valley
A dry valley may develop on many kinds of permeable rock, such as limestone and chalk, or sandy terrains that do not regularly sustain surface water flow. Such valleys do not hold surface water because it sinks into the permeable bedrock. There are many examples of chalk dry valleys along the North and South Downs in Southern England. Notably the National Trust-owned Devil's Dyke near Brighton covers some of downland scarp, and includes the deepest dry valley in the world – created when melting water eroded the chalk downland to the permafrost layer after the last ice age. The three-quarter mile long curved dry valley is around in height and attracts tourists with its views of Sussex, Hampshire and Kent. Other examples include the Alkham Valley near Dover, and the Hartley Bottom and Fawkham valleys near Dartford in north Kent. There are many examples of limestone dry valleys in the Peak District and the Yorkshire Wolds. A notable example is the valley of the River Manifold ...
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