|
Welton Oil Field
The East Midlands Oil Province, also known as the East Midlands Petroleum Province, covers the petroliferous geological area across the north-eastern part of the East Midlands of England that has a few small oil fields. The largest field in the province is the Welton oil field, the second largest onshore oil field in the UK. Geography It comprises Lincolnshire, North Lincolnshire, Nottinghamshire and northern Leicestershire. History UK oil production The UK's first oil field was discovered in the East Midlands, at Hardstoft in east Derbyshire in 1919. Prior to this, from 1851, oil shale in the Midland Valley in Scotland was used, until 1962. With North Sea oil, Britain became self-sufficient with oil and became a net exporter of oil in 1981, with exports peaking in 1985 and production peaking in 1999. The UK became a net exporter of gas in 1997 and a net importer of gas in 2004, and also a net importer of oil in 2004. UK consumption of petroleum increases each year. Per cap ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
East Midlands
The East Midlands is one of nine official regions of England at the first level of ITL for statistical purposes. It comprises the eastern half of the area traditionally known as the Midlands. It consists of Leicestershire, Derbyshire, Lincolnshire (except North and North East Lincolnshire), Northamptonshire, Nottinghamshire and Rutland. The region has an area of , with a population over 4.5 million in 2011. The most populous settlements in the region are Derby, Leicester, Lincoln, Mansfield, Northampton and Nottingham. Other notable settlements include Boston, Buxton, Chesterfield, Corby, Coalville, Gainsborough, Glossop, Grantham, Hinckley, Kettering, Loughborough, Louth, Market Harborough, Matlock, Newark-on-Trent, Oakham, Skegness, Wellingborough and Worksop. With a sufficiency-level world city ranking, Nottingham is the only settlement in the region to be classified by the Globalization and World Cities Research Network. The region is primarily served ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eakring
Eakring is a village and civil parish in the Newark and Sherwood district of Nottinghamshire, England. Its population at the 2011 Census was 419. There was sizeable oil production there in the mid-20th century. Geography The village lies between the A617 road, A617 and the A616 road, A616 roads between Ollerton and Southwell, Nottinghamshire, Southwell. Dukes Wood to the south is situated on the top of an escarpment, giving good views over the Trent valley to the east and towards Southwell to the south. Clouds formed by the Cottam Power Station are often seen on clear days to the north-east. A steep hill descends into the village from the south, on which the road passes a large residential training centre for National Grid plc. Heritage The village pub is the ''Savile Arms'' in Bilsthorpe Road. The Robin Hood Way, a long-distance footpath that passes through the village, is altogether 168 km (104 miles) long. Eakring Mill was a five-storey brick windmill, tower windmill, bu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Torksey
__NOTOC__ Torksey is a small village in the West Lindsey district of Lincolnshire, England. The population of the civil parish at the 2011 census was 875. It is situated on the A156 road, south of Gainsborough and north-west of the city of Lincoln, and on the eastern bank of the tidal River Trent, which here forms the boundary with Nottinghamshire. It is notable historically as the site of a Roman canal, a major Viking camp, the late medieval Torksey Castle and the Torksey Viaduct. History Foss Dyke, a Roman canal constructed in or about the 2nd century, joins the River Trent by way of a series of lock-gates about half a mile (800 m) south of the village. During the 9th century, Torksey was part of the Anglo-Saxon Kingdom of Lindsey. In the late 860s, a Viking invasion force known to the English as the "Great Heathen Army" conquered eastern England. In 871–2, the Vikings established a winter camp in London, but returned to Northumbria soon afterwards, following a rebe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Corringham, Lincolnshire
Corringham is a civil parish in the West Lindsey district of Lincolnshire, England. It is situated east of Gainsborough and south of Scunthorpe. Corringham comprises the two contiguous villages of Great Corringham and Little Corringham and at the 2011 census had a recorded population of 523. The hamlet of Yawthorpe lies due east of the village, and that of Bonsdale to the north. Gowin Knight, the first principal librarian of the British Museum was born here in 1713. References External links *Corringham (Great and Little Corringham) Genuki GENUKI is a genealogy web portal, run as a charitable trust. It "provides a virtual reference library of genealogical information of particular relevance to the UK and Ireland". It gives access to a large collection of information, with the emphas ....org.uk {{authority control Villages in Lincolnshire Civil parishes in Lincolnshire West Lindsey District ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dinantian
Dinantian is the name of a series (stratigraphy), series or Epoch (reference date), epoch from the Lower Carboniferous system (stratigraphy), system in Europe. It can stand for a series of rocks in Europe or the time span in which they were deposited. The Dinantian is equal to the lower part of the Mississippian age, Mississippian series in the international geologic timescale of the International Commission on Stratigraphy, ICS. The Dinantian is named for the Belgian city of Dinant where strata of this age occur. The name is still used among European geologists. Earlier terms for the Dinantian were Bernician Series, Bernician from the Anglo-Scottish borderland, and Avonian (divided into upper (Kidwellian) and lower (Clevedonian) substages) from Kidwelly on the Welsh and Clevedon on the English sides of the Bristol Channel. References {{Geological history, p, p, state=collapsed Mississippian geochronology Carboniferous Europe Stratigraphy of Europe Carboniferous Ireland ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Silesian (series)
The Silesian is in the geologic timescale of Europe a series or epoch, a subdivision of the Carboniferous system or period. It was named for Silesia, a region that stretches over the Czech Republic, Poland and Germany. Geology It follows or lies on top of the Dinantian epoch/series and lasted from roughly 326.4 to 299.0 Ma ago. The base of the Silesian is undefined, the top is defined by the first appearance of the conodont '' Streptognathodus isolatus''. Subdivisions The Silesian is subdivided into three stages, from young (upper) to old (lower): * Stephanian * Westphalian * Namurian The Namurian is a stage in the regional stratigraphy of northwest Europe with an age between roughly 326 and 313 Ma (million years ago). It is a subdivision of the Carboniferous system or period and the regional Silesian series. The Namurian is .... See also * * References {{Geological history, p, p, state=collapsed Mississippian geochronology Pennsylvanian geochronology Carbonifero ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rift
In geology, a rift is a linear zone where the lithosphere is being pulled apart and is an example of extensional tectonics. Typical rift features are a central linear downfaulted depression, called a graben, or more commonly a half-graben with normal faulting and rift-flank uplifts mainly on one side. Where rifts remain above sea level they form a rift valley, which may be filled by water forming a rift lake. The axis of the rift area may contain volcanic rocks, and active volcanism is a part of many, but not all, active rift systems. Major rifts occur along the central axis of most mid-ocean ridges, where new oceanic crust and lithosphere is created along a divergent boundary between two tectonic plates. ''Failed rifts'' are the result of continental rifting that failed to continue to the point of break-up. Typically the transition from rifting to spreading develops at a triple junction where three converging rifts meet over a hotspot. Two of these evolve to the poi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carboniferous
The Carboniferous ( ) is a geologic period and system of the Paleozoic that spans 60 million years from the end of the Devonian Period million years ago ( Mya), to the beginning of the Permian Period, million years ago. The name ''Carboniferous'' means "coal-bearing", from the Latin '' carbō'' ("coal") and '' ferō'' ("bear, carry"), and refers to the many coal beds formed globally during that time. The first of the modern 'system' names, it was coined by geologists William Conybeare and William Phillips in 1822, based on a study of the British rock succession. The Carboniferous is often treated in North America as two geological periods, the earlier Mississippian and the later Pennsylvanian. Terrestrial animal life was well established by the Carboniferous Period. Tetrapods (four limbed vertebrates), which had originated from lobe-finned fish during the preceding Devonian, became pentadactylous in and diversified during the Carboniferous, including early amphibian line ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Trafalgar House (company)
Trafalgar House was a British conglomerate with interests in property investment, property development, engineering, construction, shipping, hotels, energy and publishing. It was listed on the London Stock Exchange and was a constituent of the FTSE 100 Index but eventually floundered in the mid-1990s. History Trafalgar House was founded by entrepreneur Nigel Broackes, whose interests in share dealing and small scale property development brought him into contact with the directors of the Eastern International Investment Trust, a small trust quoted on the London Stock Exchange. In 1959, Broackes acquired a 42 per cent holding in Eastern's property subsidiary, Eastern International Property Investments (EIPI). Two years later, Broackes formed a relationship with Commercial Union which bought shares in EIPI and prepared to act as a financial backer for new property developments. Almost immediately EIPI bought a 55 per cent stake in CU's residential property subsidiary Westminster & ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alick Buchanan-Smith (politician)
Alick Laidlaw Buchanan-Smith (8 April 1932 – 29 August 1991) was a Scottish Conservative and Unionist politician. The second son of Alick Buchanan-Smith, Baron Balerno and Mary Kathleen Smith, he was educated at Edinburgh Academy, Glenalmond College, Pembroke College, Cambridge and University of Edinburgh. He was commissioned into the Gordon Highlanders and did his National Service from 1951. He was unsuccessful parliamentary candidate for West Fife in 1959, and sat as member for North Angus and Mearns from 1964 to 1983 and for Kincardine and Deeside from 1983 until his death. He was Parliamentary Under-Secretary of State for Scotland from 1970 to 1974, Minister of State for Agriculture, Fisheries and Food from 1979 to 1983, and Minister of State for Energy from 1983 to 1987. He was appointed a Privy Counsellor in 1981. Following the Conservative's defeat in the February 1974 general election he became Shadow Secretary of State for Scotland under Edward Heath. When Margar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saunders_Quarry-1.jpg "Click for more on -> Sandstone")
