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Brickhill
Brickhill is a civil parish and electoral ward within northern Bedford in Bedfordshire, England. The boundaries of Brickhill are approximately Kimbolton Road to the east, Bedford Park and the old Bedford cemetery to the south, with Cemetery Hill and the Manton Heights Industrial Estate to the west. The Woodlands Park housing estate (off Tyne Crescent) became part of Brickhill parish in 2015. History The name 'Brickhill' derives from 'Brickhill Farm' which occupied the land before the area was developed. 'Brickhill' may have been a reference to brick-making in the area, as the neighbourhood has a high clay content in its soils. Brick-making used to be a major industry in Bedfordshire (See Stewartby). The name may also derive from a compound of Brythonic and Anglo Saxon origins, which is a common occurrence in this part of the country. The Brythonic ''breg'' means 'hill', and the Anglo Saxon ''hyll'' also means 'hill'. Brickhill Farm was the location of Brickhill House, a 17th ...
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Borough Of Bedford
The Borough of Bedford is a unitary authority area with borough status in the ceremonial county of Bedfordshire, England. Its council is based in Bedford, its namesake and principal settlement, which is the county town of Bedfordshire. The borough contains one large urban area, the 71st largest in the United Kingdom that comprises Bedford and the adjacent town of Kempston, surrounded by a rural area with many villages. 75% of the borough's population live in the Bedford Urban Area and the five large villages which surround it, which makes up slightly less than 6% of the total land area of the Borough. The borough is also the location of the Wixams new town development, which received its first residents in 2009. Formation The ancient borough of Bedford was a borough by prescription, with its original date of incorporation unknown. The earliest surviving charter was issued c. 1166 by Henry II, confirming to the borough the liberties and customs which it had held in the reign ...
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Bedford
Bedford is a market town in Bedfordshire, England. At the 2011 Census, the population of the Bedford built-up area (including Biddenham and Kempston) was 106,940, making it the second-largest settlement in Bedfordshire, behind Luton, whilst the Borough of Bedford had a population of 157,479. Bedford is also the historic county town of Bedfordshire. Bedford was founded at a ford on the River Great Ouse and is thought to have been the burial place of King Offa of Mercia, who is remembered for building Offa's Dyke on the Welsh border. Bedford Castle was built by Henry I of England, Henry I, although it was destroyed in 1224. Bedford was granted borough status in 1165 and has been represented in Parliament since 1265. It is known for its large Italians in the United Kingdom, population of Italian descent. History The name of the town is believed to derive from the name of a Saxon chief called Beda, and a Ford (crossing), ford crossing the River Great Ouse. Bedford was a marke ...
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Bedford (UK Parliament Constituency)
Bedford is a United Kingdom constituencies, constituency represented in the House of Commons of the United Kingdom, House of Commons of the Parliament of the United Kingdom, UK Parliament since 2017 United Kingdom general election, 2017 by Mohammad Yasin (politician), Mohammad Yasin of the Labour Party (UK), Labour Party. The seat dates to the earliest century of regular parliaments, in 1295; its double representation was halved in 1885, then being altered by the later-termed Representation of the People Act, Fourth Reform Act in 1918. Constituency profile ;Geographical and economic profile Bedford is a marginal seat between the Labour Party (UK), Labour Party and the Conservative Party (UK), Conservatives. The main settlement is Bedford, a well-developed town centre with a considerable amount of social housing relative to Bedfordshire and higher poverty index but on a fast railway link to London and other destinations, the town is at the north end of the Thameslink (route), ...
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Biddenham International School And Sports College
Biddenham International School and Sports College (formerly John Howard Upper School) is a Mixed-sex education, mixed secondary school and sixth form located in Biddenham in the English county of Bedfordshire. The school serves the Brickhill, Harpur and Queens Park, Bedford, Queens Park areas of Bedford as well as the villages of Biddenham and Great Denham. The school holds Specialist Sports College status. History It was established in 1979 as John Howard (prison reformer), John Howard Upper School (for pupils ages 13 to 18). The headmaster for the entire time the school was as John Howard Upper School was Roy Grace. In 1988 the school was merged with Pilgrim Upper to form Biddenham Upper School on the John Howard site. Garry Fitzhugh took over as head when the merger was complete. In October 2008 Biddenham Upper School was awarded International School status by the British Council. The award was made in recognition of Biddenham's international ethos and its links with schools ...
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Ward (politics)
A ward is a local authority area, typically used for electoral purposes. In some countries, wards are usually named after neighbourhoods, thoroughfares, parishes, landmarks, geographical features and in some cases historical figures connected to the area (e.g. William Morris Ward in the London Borough of Waltham Forest, England). It is common in the United States for wards to simply be numbered. Origins The word “ward”, for an electoral subdivision, appears to have originated in the Wards of the City of London, where gatherings for each ward known as “wardmotes” have taken place since the 12th century. The word was much later applied to divisions of other cities and towns in England and Wales and Ireland. In parts of northern England, a ''ward'' was an administrative subdivision of a county, very similar to a hundred in other parts of England. Present day In Australia, Canada, New Zealand, Sri Lanka, South Africa, the United Kingdom, and the United States, wards are an ...
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Oxford Clay
The Oxford Clay (or Oxford Clay Formation) is a Jurassic marine sedimentary rock formation underlying much of southeast England, from as far west as Dorset and as far north as Yorkshire. The Oxford Clay Formation dates to the Jurassic, specifically, the Callovian and Oxfordian ages, and comprises two main facies. The lower facies comprises the Peterborough Member, a fossiliferous organic-rich mudstone. This facies and its rocks are commonly known as lower Oxford Clay. The upper facies comprises the middle Oxford Clay, the Stewartby Member, and the upper Oxford Clay, the Weymouth Member. The upper facies is a fossil poor assemblage of calcareous mudstones. Oxford Clay appears at the surface around Oxford, Peterborough and Weymouth and is exposed in many quarries around these areas. The top of the Lower Oxford Clay shows a lithological change, where fissile shale changes to grey mudstone. The Middle and Upper Oxford Clays differ slightly, as they are separated by an argillaceou ...
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Upper School
Upper schools in the UK are usually schools within secondary education. Outside England, the term normally refers to a section of a larger school. England The three-tier model Upper schools are a type of secondary school found in a minority of English local education authorities. Whilst most areas in England use a two-tier educational system – primary (ages 5–11) and secondary (ages 11–16 or 11–18 if they operate a sixth form) – counties such as Leicestershire, and Suffolk use a three-tier system of lower (ages 5–9 or 10), middle (ages 9 to 13 or 14), and Upper schools (ages 13 or 14 to 16, or 18 if they include Years 12 and 13, known as a Sixth form). The introduction of such systems began in Leicestershire in 1957. West Yorkshire followed in 1963, but the system has gradually been withdrawn in some areas since the introduction of the National Curriculum. This is because of the nature of the curriculum, which is divided into Key Stages which do not fully align wi ...
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Comprehensive School
A comprehensive school typically describes a secondary school for pupils aged approximately 11–18, that does not select its intake on the basis of academic achievement or aptitude, in contrast to a selective school system where admission is restricted on the basis of selection criteria, usually academic performance. The term is commonly used in relation to England and Wales, where comprehensive schools were introduced as state schools on an experimental basis in the 1940s and became more widespread from 1965. They may be part of a local education authority or be a self governing academy or part of a multi-academy trust. About 90% of English secondary school pupils attend a comprehensive school (academy schools, community schools, faith schools, foundation schools, free schools, studio schools, university technical colleges, state boarding schools, City Technology Colleges, etc). Specialist schools may also select up to 10% of their intake for aptitude in their specialism. A sc ...
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Grammar School
A grammar school is one of several different types of school in the history of education in the United Kingdom and other English-speaking countries, originally a school teaching Latin, but more recently an academically oriented secondary school, differentiated in recent years from less academic secondary modern schools. The main difference is that a grammar school may select pupils based on academic achievement whereas a secondary modern may not. The original purpose of medieval grammar schools was the teaching of Latin. Over time the curriculum was broadened, first to include Ancient Greek, and later English and other European languages, natural sciences, mathematics, history, geography, art and other subjects. In the late Victorian era grammar schools were reorganised to provide secondary education throughout England and Wales; Scotland had developed a different system. Grammar schools of these types were also established in British territories overseas, where they have evolv ...
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River Tyne
The River Tyne is a river in North East England. Its length (excluding tributaries) is . It is formed by the North Tyne and the South Tyne, which converge at Warden Rock near Hexham in Northumberland at a place dubbed 'The Meeting of the Waters'. The Tyne Rivers Trust measure the whole Tyne catchment as , containing of waterways. Course North Tyne The North Tyne rises on the Scottish border, north of Kielder Water. It flows through Kielder Forest, and in and out of the border. It then passes through the village of Bellingham before reaching Hexham. South Tyne The South Tyne rises on Alston Moor, Cumbria and flows through the towns of Haltwhistle and Haydon Bridge, in a valley often called the Tyne Gap. Hadrian's Wall lies to the north of the Tyne Gap. Coincidentally, the source of the South Tyne is very close to those of the Tees and the Wear. The South Tyne Valley falls within the North Pennines Area of Outstanding Natural Beauty (AONB) – the second largest of the ...
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River Waveney
The River Waveney is a river which forms the boundary between Suffolk and Norfolk, England, for much of its length within The Broads. The "ey" part of the name means "river" thus the name is tautological. Course The source of the River Waveney is a ditch on the east side of the B1113 road between the villages of Redgrave, Suffolk and South Lopham, Norfolk. The ditch on the other side of the road is the source of the River Little Ouse which continues the county boundary and, via the Great Ouse, reaches the sea at King's Lynn. It is thus claimed that during periods of heavy rainfall Norfolk can be considered to be an island. The explanation of this oddity is that the valley in which the rivers rise was formed not by these rivers, but by water spilling from the periglacial lake known as Lake Fenland. This was a periglacial lake of the Devensian glacial period, fifteen or twenty thousand years ago. The ice sheet closed the natural drainage from the Vale of Pickering, the Humber a ...
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River Avon (Warwickshire)
The River Avon () in central England flows generally southwestwards and is a major left-bank tributary of the River Severn, of which it is the easternmost. It is also known as the Warwickshire Avon or Shakespeare's Avon, to distinguish it from several other rivers of the same name in the United Kingdom. Beginning in Northamptonshire, the river flows through or adjoining the counties of Leicestershire, Northamptonshire, Warwickshire, Worcestershire and Gloucestershire, near the Cotswold Hills area. Notable towns it flows through include Rugby, Warwick, Stratford-upon-Avon, Evesham, Pershore and Tewkesbury, where it joins the Severn. It has traditionally been divided since 1719 into the Lower Avon, below Evesham, and the Upper Avon, from Evesham to above Stratford-upon-Avon. Improvements to aid navigation began in 1635, and a series of locks and weirs made it possible to reach Stratford, and to within of Warwick. The Upper Avon was tortuous and prone to flooding, and was aban ...
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