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River Brent
The River Brent is a river in west and northwest London, England, and a tributary of the River Thames. in length, it rises in the London Borough of Barnet, Borough of Barnet and flows in a generally south-west direction before joining the Tideway stretch of the Thames at Brentford. Hydronymy and etymology A letter from the Bishop of London in 705 suggesting a meeting at Breġuntford, now Brentford, is the earliest record of this place and probably therefore that of the river, suggesting that the name may be related to the Celtic languages, Celtic *''brigant-'' meaning "high" or "elevated", perhaps linked to the goddess Brigantia (goddess), Brigantia.Canham, Roy; Glanville G H (1978). ''A London Museum Archaeological Report: 2000 years of Brentford''. Ch 2; pg 3. Her Majesty's Stationery Office. Topography, geology and evolution of the Brent catchment area (For the purposes of this section, the Brent catchment area is taken to include the catchment areas of all its tributa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] [Amazon] |
Hendon
Hendon is an urban area in the London Borough of Barnet, northwest London northwest of Charing Cross. Hendon was an ancient Manorialism, manor and parish in the county of Middlesex and a former borough, the Municipal Borough of Hendon; it has been part of Greater London since 1965. Hendon falls almost entirely within the NW4 postcode, while the West Hendon part falls in NW9. Colindale to the northwest was once considered part of Hendon but is today separated by the M1 motorway. The district is most famous for the London Aerodrome which later became the RAF Hendon; from 1972 the site of the RAF station was gradually handed over to housing development and to the Royal Air Force Museum London, RAF Museum. The railways reached Hendon in 1868 with Hendon railway station, Hendon station on the Midland Main Line, followed by the London Underground further east under the name Hendon Central tube station, Hendon Central in 1923. Brent Street emerged as its commercial centre by the 1890s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] [Amazon] |
Brentford
Brentford is a suburban town in West (London sub region), West London, England and part of the London Borough of Hounslow. It lies at the confluence of the River Brent and the River Thames, Thames, west of Charing Cross. Its economy has diverse company headquarters buildings which mark the start of the M4 corridor; in transport it also has two railway stations and Boston Manor tube station, Boston Manor Underground station on its northwest border with Hanwell. Brentford has a convenience shopping and dining venue grid of streets at its centre. Brentford at the start of the 21st century attracted regeneration of its little-used warehouse premises and docks including the remodelling of the waterfront to provide more economically active shops, townhouses and apartments, some of which comprise Brentford Dock. A 19th- and 20th-century mixed social and private housing locality, New Brentford is contiguous with the Osterley neighbourhood of Isleworth and Syon Park and the Great Wes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] [Amazon] |
Mutton Brook
__NOTOC__ Mutton Brook is a stream which runs between East Finchley and Hendon in the London Borough of Barnet. It is a tributary of the River Brent, which is itself a tributary of the River Thames. The brook rises in Cherry Tree Wood and flows underground to emerge at the back of Belvedere Court, Lyttleton Road. It then passes under Lyttleton Road and flows along the south side of the road and Falloden Way through Lyttleton Playing Fields, Fletchers Gardens and Northway Gardens. Near Brookland Rise, it crosses briefly to the north side of Falloden Way before crossing back to Brookside Walk. It passes under Finchley Road at Henlys Corner and then under the North Circular Road to meet Dollis Brook close to Bridge Lane. The two brooks then become the River Brent. The brook is confined in a concrete or wood channel along the whole of its length, and the water quality is often poor. However, from Lyttleton Playing Fields to the junction with Dollis Brook its route is almost all th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] [Amazon] |
Pleistocene
The Pleistocene ( ; referred to colloquially as the ''ice age, Ice Age'') is the geological epoch (geology), epoch that lasted from to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was finally confirmed in 2009 by the International Union of Geological Sciences, the cutoff of the Pleistocene and the preceding Pliocene was regarded as being 1.806 million years Before Present (BP). Publications from earlier years may use either definition of the period. The end of the Pleistocene corresponds with the end of the last glacial period and also with the end of the Paleolithic age used in archaeology. The name is a combination of Ancient Greek () 'most' and (; Latinized as ) 'new'. The aridification and cooling trends of the preceding Neogene were continued in the Pleistocene. The climate was strongly variable depending on the glacial cycle, oscillating between cold Glacial period, glacial periods and warmer Interglacial, int ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] [Amazon] |
Bagshot Formation
In geology, the Bagshot Beds are a series of sands and clays of shallow-water origin, some being fresh-water, some marine. They belong to the upper Eocene formation of the London and Hampshire basins, in England and derive their name from Bagshot Heath in Surrey. They are also well developed in Hampshire, Berkshire and the Isle of Wight. The following divisions are generally accepted: *Upper Bagshot Beds — Barton sand and Barton clay. *Middle Bagshot Beds — Bracklesham Beds. *Lower Bagshot Beds — Bournemouth Beds and Alum Bay Beds. The lower division consists of pale-yellow, current-bedded sand and loam, with layers of pipeclay and occasional beds of flint pebbles. In the London basin, wherever the junction of the Bagshot beds with the London clay is exposed, it is clear that no sharp line can be drawn between these formations. The Lower Bagshot Beds may be observed at Brentwood, Billericay and High Beach in Essex; outliers, capping hills of London clay, occur at Ha ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] [Amazon] |
Highgate
Highgate is a suburban area of N postcode area, north London in the London Borough of Camden, London Boroughs of Camden, London Borough of Islington, Islington and London Borough of Haringey, Haringey. The area is at the north-eastern corner of Hampstead Heath, north-northwest of Charing Cross. Highgate is one of the most expensive London suburbs in which to live. It has three conservation organisations: the Highgate Society, the Highgate Neighbourhood Forum and the Highgate Conservation Area Advisory Committee, to protect and enhance its character and amenities. Until late Victorian times, it was a distinct village outside London, sitting astride the main road to the north. The area retains many green expanses, including the eastern part of Hampstead Heath, three ancient woods, Waterlow Park and the eastern-facing slopes, known as Highgate bowl. At its centre is Highgate village, largely a collection of Georgian architecture, Georgian shops, pubs, restaurants and residenti ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] [Amazon] |
Hampstead
Hampstead () is an area in London, England, which lies northwest of Charing Cross, located mainly in the London Borough of Camden, with a small part in the London Borough of Barnet. It borders Highgate and Golders Green to the north, Belsize Park to the south and is surrounded from the northeast by Hampstead Heath, a large, hilly expanse of parkland. Hampstead is known for its intellectual, artistic, liberal, and literary associations. It contains a number of listed buildings, such as Burgh House, Kenwood House, the Spaniard's Inn, and the Everyman cinema. With some of the most expensive housing in London, Hampstead has had many notable residents, both past and present, including King Constantine II of Greece and his wife Queen Anne Marie, Helena Bonham Carter, Agatha Christie, T. S. Eliot, Jon English, Sigmund Freud, Stephen Fry, Ricky Gervais, Jim Henson, George Orwell, Harry Styles and Elizabeth Taylor. As of 2004, Hampstead has been home to more Prime Mini ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] [Amazon] |
Harrow On The Hill
Harrow on the Hill or Harrow-on-the-Hill is a locality and historic village in the borough of London Borough of Harrow, Harrow in Greater London, England. The name refers to Harrow Hill, ,Mills, A., ''Dictionary of London Place Names'', (2001) and is located some half a mile south of the modern Harrow, London, town of Harrow. The village dates back to early Middle Ages, medieval times, built around the 11th-century St Mary's Church, Harrow on the Hill, St Mary's Church, and is the location of Harrow School, Harrow, St Dominic's Sixth Form College, St Dominic's and The John Lyon School, John Lyon schools. Etymology Etymology before 1398 derives from Harrow, London, Harrow, & The Saxon Chronicles/The Peterborough Chronicle, which first recorded Harrow Hill in 767 as ''Gumeninga Hergae''. A suggested meaning is "heathen temple" of a tribe called the 'Gumeningas', sons of Gumen. One of the earliest recorded uses of the name is found in 1398 as ''Harrowe atte Hille''. The hill has h ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] [Amazon] |
London Clay
The London Clay Formation is a Sediment#Shores and shallow seas, marine formation (geology), geological formation of Ypresian (early Eocene Epoch, c. 54-50 million years ago) age which outcrop, crops out in the southeast of England. The London Clay is well known for its fossil content. The fossils from the lower Eocene rocks indicate a moderately warm climate, the tropical or subtropical flora. Though sea levels changed during the deposition of the clay, the habitat was generally a lush forest – perhaps like in Indonesia or East Africa today – bordering a warm, shallow ocean. The London Clay is a stiff bluish clay which becomes brown when weathered and oxidized. Nodular lumps of pyrite are frequently found in the clay layers. Pyrite was produced by microbial activity (sulfate reducing bacteria) during clay sedimentation. Once clay is exposed to atmospheric oxygen, framboidal pyrite with a great specific surface is rapidly oxidized. Acid mine drainage, Pyrite oxidation produce ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] [Amazon] |
Eocene
The Eocene ( ) is a geological epoch (geology), epoch that lasted from about 56 to 33.9 million years ago (Ma). It is the second epoch of the Paleogene Period (geology), Period in the modern Cenozoic Era (geology), Era. The name ''Eocene'' comes from the Ancient Greek (''Ēṓs'', 'Eos, Dawn') and (''kainós'', "new") and refers to the "dawn" of modern ('new') fauna that appeared during the epoch.See: *Letter from William Whewell to Charles Lyell dated 31 January 1831 in: * From p. 55: "The period next antecedent we shall call Eocene, from ήως, aurora, and χαινος, recens, because the extremely small proportion of living species contained in these strata, indicates what may be considered the first commencement, or ''dawn'', of the existing state of the animate creation." The Eocene spans the time from the end of the Paleocene Epoch to the beginning of the Oligocene Epoch. The start of the Eocene is marked by a brief period in which the concentration of the carbon isoto ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] [Amazon] |
London Basin
The London Basin is an elongated, roughly triangular sedimentary basin approximately long which underlies London and a large area of south east England, south eastern East Anglia and the adjacent North Sea. The basin formed as a result of compressional tectonics related to the Alpine orogeny during the Palaeogene period and was mainly active between 40 and 60 million years ago. Boundaries and shape Spatial boundaries The generally accepted boundaries are the Late Cretaceous Chalk Group's escarpments of the Chilterns and Marlborough Downs to the north and the North Downs and Berkshire Downs to the south. To the south lie the Weald and Salisbury Plain and to the north is the Vale of Aylesbury. The approximate western limit is in the Marlborough area of Wiltshire. The eastern end merges with the North Sea Basin, extending on land along the north Kent coast to Reculver and up the east coast of Essex and into Suffolk, where it is overlain by Pleistocene 'Crag' deposits w ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] [Amazon] |
Brent Catchment Topography
Brent may refer to: *Brent (name), an English given and surname Place name ;In the United States *Brent, Alabama *Brent, Florida * Brent, Georgia *Brent, Missouri, a ghost town *Brent, Oklahoma ;In the United Kingdom * Brent, Cornwall * Brent Knoll, a hill in Somerset, England *Brent Knoll (village), a village at the foot of the hill *East Brent, another village at the foot of the hill *London Borough of Brent, England ** Brent (electoral division), Greater London Council *South Brent, Devon, England ;Elsewhere *Brent, Ontario, a village in Algonquin Provincial Park, Canada * Brent crater, a meteor crater named after the village of Brent, Ontario *Brent oilfield, North Sea In fiction * Brent (''Planet of the Apes'') * Corey Brent, fictional character on the ITV soap opera ''Coronation Street'' * David Brent, fictional character on the BBC television comedy ''The Office'' * Stefan Brent, fictional character on the ITV soap opera ''Coronation Street'' * Brent Scopes, fiction ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] [Amazon] |
