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Child Okeford
Child Okeford (sometimes written Childe Okeford) is a village and civil parish in the county of Dorset in southern England, east of the small town of Sturminster Newton in the North Dorset administrative district. Child Okeford lies downstream from Sturminster, along the River Stour, which passes half a mile west of the village. In the 2011 census the civil parish had a population of 1,114. History On Hambledon Hill to the east of the village are a Neolithic ceremonial burial site and an Iron Age hill fort. The latter has multiple ramparts enclosing and is rich in occupation remains. It occupies the entire northern spur of the hill above and has been described as "one of the most impressive earthworks in southern England". In the Domesday Book of 1086 Child Okeford was recorded as ''Acford'' and appears in two entries. It had 39 households and a total taxable value of 10 geld units. By 1227 the village was known as ''Childacford''. The village's name derives from the Old ...
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Office For National Statistics
The Office for National Statistics (ONS; cy, Swyddfa Ystadegau Gwladol) is the executive office of the UK Statistics Authority, a non-ministerial department which reports directly to the UK Parliament. Overview The ONS is responsible for the collection and publication of statistics related to the economy, population and society of the UK; responsibility for some areas of statistics in Scotland, Northern Ireland and Wales is devolved to the devolved governments for those areas. The ONS functions as the executive office of the National Statistician, who is also the UK Statistics Authority's Chief Executive and principal statistical adviser to the UK's National Statistics Institute, and the 'Head Office' of the Government Statistical Service (GSS). Its main office is in Newport near the United Kingdom Intellectual Property Office and Tredegar House, but another significant office is in Titchfield in Hampshire, and a small office is in London. ONS co-ordinates data collection wi ...
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Compton Abbas
Compton Abbas is a village and civil parish in north Dorset, England. It lies south of the town of Shaftesbury. It is sited on greensand strata on the edge of the Blackmore Vale, below the chalk downs of Cranborne Chase. On top of these hills is Compton Abbas Airfield. The A350 road between Wiltshire and the south coast passes through the village. In the 2011 census the civil parish had a population of 216. The name ''Compton Abbas'' derives from the Saxon "cumb-ton", meaning 'village in a narrow valley', plus "abbas" which refers to Shaftesbury Abbey (the land was owned by the abbess). The church, St. Mary's, was built in 1866 to replace the older structure which was more remote from the village. The tower of the Church of St Mary in East Compton is a Grade I listed In the United Kingdom, a listed building or listed structure is one that has been placed on one of the four statutory lists maintained by Historic England in England, Historic Environment Scotland in Scotla ...
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Chalk
Chalk is a soft, white, porous, sedimentary carbonate rock. It is a form of limestone composed of the mineral calcite and originally formed deep under the sea by the compression of microscopic plankton that had settled to the sea floor. Chalk is common throughout Western Europe, where deposits underlie parts of France, and steep cliffs are often seen where they meet the sea in places such as the Dover cliffs on the Kent coast of the English Channel. Chalk is mined for use in industry, such as for quicklime, bricks and builder's putty, and in agriculture, for raising pH in soils with high acidity. It is also used for " blackboard chalk" for writing and drawing on various types of surfaces, although these can also be manufactured from other carbonate-based minerals, or gypsum. Description Chalk is a fine-textured, earthy type of limestone distinguished by its light color, softness, and high porosity. It is composed mostly of tiny fragments of the calcite shells or skeletons ...
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Gault
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 London Basin, ...
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Greensand (geology)
Greensand or green sand is a sand or sandstone which has a greenish color. This term is specifically applied to shallow marine sediment that contains noticeable quantities of rounded greenish grains. These grains are called ''glauconies'' and consist of a mixture of mixed-layer clay minerals, such as smectite and glauconite. Greensand is also loosely applied to any glauconitic sediment. Formation Greensand forms in anoxic marine environments that are rich in organic detritus and low in sedimentary input. Having accumulated in marine environments, greensands can be fossil-rich, such as in the late-Cretaceous deposits of New Jersey. Occurrence Important exposures are known from both northern and western Europe, North America, southeastern Brazil and north Africa. Well known and important greensands are the Upper and Lower Greensands of England and occur within Eocene and Cretaceous sedimentary strata underlying the coastal plains of New Jersey and Delaware. Although greensand has ...
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Kimmeridge Clay
The Kimmeridge Clay is a sedimentary deposit of fossiliferous marine clay which is of Late Jurassic to lowermost Cretaceous age and occurs in southern and eastern England and in the North Sea. This rock formation is the major source rock for North Sea oil. The fossil fauna of the Kimmeridge Clay includes turtles, crocodiles, sauropods, plesiosaurs, pliosaurs and ichthyosaurs, as well as a number of invertebrate species. Description Kimmeridge Clay is named after the village of Kimmeridge on the Dorset coast of England, where it is well exposed and forms part of the Jurassic Coast World Heritage Site. Onshore, it is of Late Jurassic (Kimmeridgian) age and outcrops across England, in a band stretching from Dorset in the south-west, north-east to North Yorkshire. Offshore, it extends into the Lower Cretaceous (Berriasian Stage) and it is found throughout the Southern, Central and Northern North Sea. The foundations of the Humber Bridge on the southern (Barton) side of the bridg ...
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Shillingstone Railway Station
Shillingstone railway station was a station on the Somerset and Dorset Joint Railway (S&DJR), serving the village of Shillingstone in the English county of Dorset. Shillingstone is the last surviving example of a station built by the Dorset Central Railway (one of the forerunners of the S&DJR). The station closed in 1966, when services were withdrawn from the S&DJR route. Since 2001, enthusiasts have been working to re-open the station as a heritage railway attraction. The main building has now been renovated, and opened to the public as a museum, shop and refreshment room in 2008. History The station was opened on 31 August 1863 by the Somerset and Dorset Railway, although planned and designed by one of its two predecessors, the Dorset Central Railway. Initial train services were provided by the London and South Western Railway (LSWR). In 1875, the Midland Railway and the LSWR together took over a joint lease of the line, forming the Somerset and Dorset Joint Railway. At t ...
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Richard Beeching
Richard Beeching, Baron Beeching (21 April 1913 – 23 March 1985), commonly known as Dr Beeching, was a physicist and engineer who for a short but very notable time was chairman of British Railways. He became a household name in Britain in the early 1960s for his report ''The Reshaping of British Railways'', commonly referred to as "The Beeching Report", which led to far-reaching changes in the railway network, popularly known as "the Beeching Axe". As a result of the report, just over were removed from the system on cost and efficiency grounds, leaving Britain with of railway lines in 1966. A further were lost by the end of the 1960s, while other lines were reduced to freight use only. Early years Beeching was born in Sheerness on the Isle of Sheppey in Kent, the second of four brothers. His father was Hubert Josiah Beeching, a reporter with the ''Kent Messenger'' newspaper, his mother a schoolteacher and his maternal grandfather a dockyard worker. Shortly after his birth, ...
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Shillingstone
Shillingstone is a village and civil parish in the Blackmore Vale area of north Dorset, England, situated on the River Stour between Sturminster Newton and Blandford Forum. In the 2011 Census the civil parish had 479 households and a population of 1,170. South of Shillingstone is a large area of woodland on Okeford and Shillingstone Hill which forms part of Blandford Forest. History Shillingstone features in the Domesday Book of 1086 as a settlement of 46 households, with meadow, woodlands and a mill, under the lordship of Ascelin. Its name is a derivation of Eschelling's (or Ascelin's) town. It once had the tallest maypole in Dorset – high. An agricultural community, it specialised in the production of moss. In the first World War, it earned the title, "the bravest village in Britain", because of the high proportion of residents who volunteered to join the armed forces. In 1924 the Shillingstone lime works was started to extract lime from the chalk beds at Shillin ...
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Somerset And Dorset Joint Railway
The Somerset and Dorset Joint Railway, also known as the S&D, SDJR or S&DJR, was an English railway line connecting Bath (in north-east Somerset) and Bournemouth (now in south-east Dorset but then in Hampshire), with a branch from Evercreech Junction to Burnham-on-Sea and Bridgwater. Strictly speaking, the main line ran from Bath Junction to Broadstone, as the line between Broadstone and Bournemouth was owned by the London and South Western Railway, while the line between Bath Junction and Bath was owned by the Midland Railway. The line was used for freight and local passenger traffic over the Mendip Hills, and for weekend holiday traffic to Bournemouth. Criticised as the "Slow and Dirty" or the "Slow and Doubtful", it closed in 1966 as part of the Beeching axe despite protests from the local community. Overview The Somerset and Dorset Railway (S&D) was created in 1862, as an amalgamation of the Somerset Central Railway and the Dorset Central Railway. By the following ye ...
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War Memorial
A war memorial is a building, monument, statue, or other edifice to celebrate a war or victory, or (predominating in modern times) to commemorate those who died or were injured in a war. Symbolism Historical usage It has been suggested that the world's earliest known war memorial is the White Monument at Tell Banat, Aleppo Governorate, Syria, which dates from the 3rd millennium BC and appears to have involved the systematic burial of fighters from a state army. The Nizari Ismailis of the Alamut period (the Assassins) had made a secret roll of honor in Alamut Castle containing the names of the assassins and their victims during their uprising. The oldest war memorial in the United Kingdom is Oxford University's All Souls College. It was founded in 1438 with the provision that its fellows should pray for those killed in the long wars with France. War memorials for the Franco-Prussian War (1870–71) were the first in Europe to have rank-and-file soldier ...
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World War I
World War I (28 July 1914 11 November 1918), often abbreviated as WWI, was one of the deadliest global conflicts in history. Belligerents included much of Europe, the Russian Empire, the United States, and the Ottoman Empire, with fighting occurring throughout Europe, the Middle East, Africa, the Pacific, and parts of Asia. An estimated 9 million soldiers were killed in combat, plus another 23 million wounded, while 5 million civilians died as a result of military action, hunger, and disease. Millions more died in genocides within the Ottoman Empire and in the 1918 influenza pandemic, which was exacerbated by the movement of combatants during the war. Prior to 1914, the European great powers were divided between the Triple Entente (comprising France, Russia, and Britain) and the Triple Alliance (containing Germany, Austria-Hungary, and Italy). Tensions in the Balkans came to a head on 28 June 1914, following the assassination of Archduke Franz Ferdin ...
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