Upper Beeding
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Upper Beeding
Upper Beeding is a village and civil parish in the Horsham District of West Sussex, England. It is located at the northern end of the River Adur gap in the South Downs, four miles (6.4 km) north of Shoreham-by-Sea and has a land area of 1877 hectares (4637 acres). The site is a bridging point over the river: on the opposite bank are Bramber and Steyning, making the whole area somewhat built-up. The civil parish also includes the smaller village of Small Dole to the north (nearer to Henfield), and the village of Edburton to the northeast. Upper Beeding is on the northern edge of the South Downs National Park which was created in 2010. The South Downs Way and Monarch's Way long-distance footpaths run through the parish; the area is popular with walkers, cyclists and equestrians. It is also at the western end of the Beeding Hill to Newtimber Hill Site of Special Scientific Interest. History The community was originally (and for the majority of its history) c ...
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United Kingdom Census 2001
A nationwide census, known as Census 2001, was conducted in the United Kingdom on Sunday, 29 April 2001. This was the 20th UK census and recorded a resident population of 58,789,194. The 2001 UK census was organised by the Office for National Statistics (ONS) in England and Wales, the General Register Office for Scotland (GROS) and the Northern Ireland Statistics and Research Agency (NISRA). Detailed results by region, council area, ward and output area are available from their respective websites. Organisation Similar to previous UK censuses, the 2001 census was organised by the three statistical agencies, ONS, GROS, and NISRA, and coordinated at the national level by the Office for National Statistics. The Orders in Council to conduct the census, specifying the people and information to be included in the census, were made under the authority of the Census Act 1920 in Great Britain, and the Census Act (Northern Ireland) 1969 in Northern Ireland. In England and Wales these re ...
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Beeding Hill To Newtimber Hill
Beeding Hill to Newtimber Hill is a biological and geological Downland Site of Special Scientific Interest (SSSI) north of Shoreham-by-Sea in West Sussex. It is a Nature Conservation Review site, Grade 2, and it includes Devil's Dyke Geological Conservation Review site. There are thirteen distinct areas within this SSSI. Most of it is on the north-facing slope of the South Downs on unimproved chalk grassland. Grazed chalk downland, such as this, has a diverse flora with around 40 flowering plants per square metre. There are areas of scrub and in places this scrub has developed into woodland, and there are also some areas of mature beech woodland. The richest areas are dominated by upright brome and fine-leaved grasses such as sheep’s fescue and crested hair-grass. The site supports rare orchid species including frog orchid and in the woodlands, yellow bird’s nest and bird’s nest orchid. The site supports a nationally important assemblage of the Opilionid group of Arachn ...
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William The Conqueror
William I; ang, WillelmI (Bates ''William the Conqueror'' p. 33– 9 September 1087), usually known as William the Conqueror and sometimes William the Bastard, was the first House of Normandy, Norman List of English monarchs#House of Normandy, king of England, reigning from 1066 until his death in 1087. A descendant of Rollo, he was Duke of Normandy from 1035 onward. By 1060, following a long struggle to establish his throne, his hold on Normandy was secure. In 1066, following the death of Edward the Confessor, William invaded England, leading an army of Normans to victory over the Anglo-Saxons, Anglo-Saxon forces of Harold Godwinson at the Battle of Hastings, and suppressed subsequent English revolts in what has become known as the Norman Conquest. The rest of his life was marked by struggles to consolidate his hold over England and his continental lands, and by difficulties with his eldest son, Robert Curthose. William was the son of the unmarried Duke Robert I of Normandy ...
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Gault Clay
The Gault Formation is a geological formation of stiff blue clay deposited in a calm, fairly deep-water marine environment during the Lower Cretaceous Period (Upper and Middle Albian). It is well exposed in the coastal cliffs at Copt Point in Folkestone, Kent, England, where it overlays the Lower Greensand formation, and underlies the Upper Greensand Formation. These represent different facies, with the sandier parts probably being deposited close to the shore and the clay in quieter water further from the source of sediment; both are believed to be shallow-water deposits. The etymology of the name is uncertain and probably of local origin. Distribution It is found in exposure on the south side of the North Downs and the north side of the South Downs. It is also to be found beneath the scarp of the Berkshire Downs, in the Vale of White Horse, in Oxfordshire, England, and on the Isle of Wight where it is known as Blue Slipper. Gault underlies the chalk beneath the Londo ...
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Lower Greensand
The Lower Greensand Group is a geological unit present across large areas of Southern England. It was deposited during the Aptian and Albian stages of the Early Cretaceous. It predominantly consists of sandstone and unconsolidated sand that were deposited in shallow marine conditions. Lithology The Lower Greensand typically comprises loose, unconsolidated sandstone (termed rubblestone/rubble in construction) and sands of varying grain size with subordinate amounts of siltstones, mudstones (containing smectites and similar) and limestones. The name "greensand" is derived from the presence of the green coloured mineral glauconite, which forms in shallow marine conditions. In the Weald of East Sussex the lowermost part of the group is recognised by green glauconitic clays with a basal bed of phosphate nodules. These clays are overlain by green sandy clays and silts and finally homogeneous fine grained sands.Lake, R.D. & Shepard-Thorn, E.R. (1987) ''Geology of the country around Ha ...
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Chalk Downland
Downland, chalkland, chalk downs or just downs are areas of open chalk hills, such as the North Downs. This term is used to describe the characteristic landscape in southern England where chalk is exposed at the surface. The name "downs" is derived from the Old English word dun, meaning "hill". Distribution The largest area of downland in southern England is formed by Salisbury Plain, mainly in Wiltshire. To the southwest, downlands continue via Cranborne Chase into Dorset as the Dorset Downs and southwards through Hampshire as the Hampshire Downs onto the Isle of Wight. To the northeast, downlands continue along the Berkshire Downs and Chiltern Hills through parts of Berkshire, Oxfordshire, Buckinghamshire, Hertfordshire, Bedfordshire and into Cambridgeshire. To the east downlands are found north of the Weald in Surrey, Kent and part of Greater London, forming the North Downs. To the southeast the downlands continue into West Sussex and East Sussex as the South Downs. Similar cha ...
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Brighton And Hove
Brighton and Hove () is a city and unitary authority in East Sussex, England. It consists primarily of the settlements of Brighton and Hove, alongside neighbouring villages. Often referred to synonymously as Brighton, the City of Brighton and Hove is England's most populous seaside resort, as well as the second most populous urban area in South East England. It is administered by Brighton and Hove City Council, which is currently in Green minority control. In 2014, Brighton and Hove City Council formed the Greater Brighton City Region with neighbouring local authorities. It can be considered both a coastal and a downland city benefiting from both the sea and the chalk hill grasslands that it is nestled in. Unification In 1992 a government commission was set up to conduct a structural review of local government arrangements across England. In its draft proposals for East Sussex, the commission suggested two separate unitary authorities be created for the towns of Brighton ...
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Fulking
Fulking is a village and civil parish in the Mid Sussex District of West Sussex, England. The parish lies wholly with the South Downs National Park. The parish is located on the north slopes of the South Downs, five miles (8 km) to the north-west of Brighton, sandwiched between the Upper Beeding and Poynings parish. The civil parish covers an area of . The downland scarp, which includes the Fulking and Perching bostals (paths), is part of the Beeding Hill to Newtimber Hill designated Site of Special Scientific Interest. History Fulking was originally part of the parish of Edburton. The parish was unusual in that part lay in Bramber rape and Burbeach hundred and part in Lewes rape and Poynings hundred (usually parish boundaries followed rape boundaries). The civil parish of Fulking was created from the eastern half of the ancient parish (sometimes referred to as 'the ecclesiastical parish') in 1894, after the creation of the administrative counties of West Sussex (which inco ...
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Woodmancote, Horsham District
Woodmancote is a village and civil parish in the Horsham District of West Sussex, England. The village is 1 mile (1.5 km) southeast of Henfield on the A281 road. It should not be confused with the other West Sussex village of Woodmancote near Chichester. This scattered community has no village centre. The parish includes the hamlet of Blackstone. The Anglican parish church, St Peter's, which stands alone beside the A281 road, dates to the thirteenth century, and was largely rebuilt in 1868. Close to the church is Woodmancote Place, a large house used as a country club. There is also a parish hall. Woodmancote is recorded in the ''Domesday Book'' of 1086 as "Odemancote". Two of the Lewes martyrs, burnt at the stake in the Marian Persecutions of 1556, Thomas Harland and John Oswald, came from Woodmancote. The parish has a land area of 849 hectares (2096 acres). In the 2001 census 478 people lived in 189 households, of whom 248 were economically active. At the ...
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Henfield
Henfield is a large village and civil parish in the Horsham District of West Sussex, England. It lies south of London, northwest of Brighton, and east northeast of the county town of Chichester at the road junction of the A281 and A2037. The parish has a land area of . In the 2001 census 5,012 people lived in 2,153 households, of whom 2,361 were economically active. Other nearby towns include Burgess Hill to the east and Shoreham-by-Sea to the south. The population at the 2011 Census was 5,349. Just west of the town, the two branches of the River Adur, the western Adur and the eastern Adur, meet at Betley Bridge. From Henfield the Adur flows on into the English Channel at Shoreham-by-Sea. Henfield was already a large village, of 52 households, at the time of Domesday (1086). Facilities One of the largest village communities in the Horsham district, Henfield has an old and attractive centre. It has a modern and intensely used village hall just off the High Street, the ...
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Hamlet (place)
A hamlet is a human settlement that is smaller than a town or village. Its size relative to a Parish (administrative division), parish can depend on the administration and region. A hamlet may be considered to be a smaller settlement or subdivision or satellite entity to a larger settlement. The word and concept of a hamlet has roots in the Anglo-Norman settlement of England, where the old French ' came to apply to small human settlements. Etymology The word comes from Anglo-Norman language, Anglo-Norman ', corresponding to Old French ', the diminutive of Old French ' meaning a little village. This, in turn, is a diminutive of Old French ', possibly borrowed from (West Germanic languages, West Germanic) Franconian languages. Compare with modern French ', Dutch language, Dutch ', Frisian languages, Frisian ', German ', Old English ' and Modern English ''home''. By country Afghanistan In Afghanistan, the counterpart of the hamlet is the Qila, qala (Dari language, Dari: ...
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