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Sydney Ewart Hollingworth
Sydney Ewart Hollingworth (7 November 1899 – 23 June 1966) was a British geologist and academic who specialized in the Pleistocene geology of northwest England, and was Professor of Geology at University College London, 1946–66. The Hollingworth Cliffs in Antarctica and the mineral "Hollingworthite" are named after him. Early life and education He was born in Flore, Northamptonshire, the son of Alice Masters Hollingworth and Charles Hollingworth, a foreman in the Army Ordnance Department. He was educated at Northampton School, and then joined the Army at the end of the First World War. He was wounded in active service. After the end of the war, he entered Clare College, Cambridge, where he was influenced by John Edward Marr and Alfred Harker. Hollingworth took first-class honours in both parts of the natural sciences tripos and in 1921 was awarded the Harkness scholarship. In 1921, he graduated from Cambridge and 10 years later earned a DSc from the University College Lond ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Flore, Northamptonshire
Flore (historically spelled as ''Floore'') is a village and civil parish in West Northamptonshire in England. The village's name means 'Floor', perhaps referring to a Roman tessellated pavement. South of the neighbouring parish of Nether Heyford such a pavement has been unearthed. Alternatively, it may refer to the situation of the village in the valley bottom of the River Nene. The A45 road divided the upper part of the village from several older, lower streets until a bypass opened on 15 November 2018. The historical village of Glassthorpe lay in the vicinity. The population at the 2001 census was 1,221, falling to 1,194 at the 2011 census. The Grade II listed Flore House was built in 1608 for the Enyon family. The thatched cottage in Flore called ''Adams Cottage''location is said to be the home of the ancestors of John Adams John Adams (October 30, 1735 – July 4, 1826) was an American statesman, attorney, diplomat, writer, and Founding Fathers of the United Sta ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Brampton, Carlisle
Brampton is a market town, civil parish and electoral ward within the City of Carlisle district of Cumbria, England, about east of Carlisle and south of Hadrian's Wall. Historically part of Cumberland, it is situated off the A69 road which bypasses it. St Martin's Church is famous as the only church designed by the Pre-Raphaelite architect Philip Webb, and contains one of the most exquisite sets of stained glass windows designed by Sir Edward Burne-Jones, and executed in the William Morris studio. History The town is thought to have been founded in the 7th century as an Anglian settlement. The place-name 'Brampton' is first attested in Charter Rolls of 1252, where it appears as ''Braunton''. In the ''Taxatio Ecclesiastica'' of 1291 it appears as ''Brampton''. The name derives from the Old English 'Brōm-tūn', meaning "town or settlement where broom grew". Its original church survives a couple of miles away to the west as Brampton Old Church, on the site of a Staneg ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sulphur
Sulfur (or sulphur in British English) is a chemical element with the symbol S and atomic number 16. It is abundant, multivalent and nonmetallic. Under normal conditions, sulfur atoms form cyclic octatomic molecules with a chemical formula S8. Elemental sulfur is a bright yellow, crystalline solid at room temperature. Sulfur is the tenth most abundant element by mass in the universe and the fifth most on Earth. Though sometimes found in pure, native form, sulfur on Earth usually occurs as sulfide and sulfate minerals. Being abundant in native form, sulfur was known in ancient times, being mentioned for its uses in ancient India, ancient Greece, China, and ancient Egypt. Historically and in literature sulfur is also called brimstone, which means "burning stone". Today, almost all elemental sulfur is produced as a byproduct of removing sulfur-containing contaminants from natural gas and petroleum.. Downloahere The greatest commercial use of the element is the production o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Iron Ore
Iron ores are rocks and minerals from which metallic iron can be economically extracted. The ores are usually rich in iron oxides and vary in color from dark grey, bright yellow, or deep purple to rusty red. The iron is usually found in the form of magnetite (, 72.4% Fe), hematite (, 69.9% Fe), goethite (, 62.9% Fe), limonite (, 55% Fe) or siderite (, 48.2% Fe). Ores containing very high quantities of hematite or magnetite (greater than about 60% iron) are known as "natural ore" or "direct shipping ore", meaning they can be fed directly into iron-making blast furnaces. Iron ore is the raw material used to make pig iron, which is one of the main raw materials to make steel—98% of the mined iron ore is used to make steel. In 2011 the ''Financial Times'' quoted Christopher LaFemina, mining analyst at Barclays Capital, saying that iron ore is "more integral to the global economy than any other commodity, except perhaps oil". Sources Metallic iron is virtually unknown on ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Northampton Sand Formation
The Northampton Sand Formation, sometimes called the Northamptonshire Sand, is a Middle Jurassic geological formation which is placed within the Inferior Oolite Group. It was formerly worked extensively in Northamptonshire for its ironstone. The Northampton Sand Formation constitutes the lowest part of the Inferior Oolite Group and lies on the upper Lias clay. It attains a maximum thickness of up to to the north and west of Northampton where it lies in a subterranean basin. In the south, it fades out around Towcester. Northward from the edge of the basin in the upper Lias, under Northampton, it lies progressively lower beneath the Jurassic Lincolnshire limestones. A little to the north of Corby Glen () it is at about from the surface. It fades out under north Lincolnshire as the strata rise towards the Market Weighton Axis. The formation to dates to the Aalenian, and predominantly consists of sandy ironstone, which when freshly exposed is greenish-grey in colour, which weath ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ironstone
Ironstone is a sedimentary rock, either deposited directly as a ferruginous sediment or created by chemical replacement, that contains a substantial proportion of an iron ore compound from which iron (Fe) can be smelted commercially. Not to be confused with native or telluric iron, which is very rare and found in metallic form, the term ''ironstone'' is customarily restricted to hard, coarsely banded, non-banded, and non-cherty sedimentary rocks of post-Precambrian age. The Precambrian deposits, which have a different origin, are generally known as banded iron formations. The iron minerals comprising ironstones can consist either of oxides, i.e. limonite, hematite, and magnetite; carbonates, i.e. siderite; silicates, i.e. chamosite; or some combination of these minerals.U.S. Bureau of Mines Staff (1996) ''Dictionary of Mining, Mineral, & Related Terms.'' Report SP-96-1, U.S. Department of Interior, U.S. Bureau of Mines, Washington, D.C.Neuendorf, K. K. E., J. P. Mehl Jr., and J. A. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jurassic
The Jurassic ( ) is a Geological period, geologic period and System (stratigraphy), stratigraphic system that spanned from the end of the Triassic Period million years ago (Mya) to the beginning of the Cretaceous Period, approximately Mya. The Jurassic constitutes the middle period of the Mesozoic, Mesozoic Era and is named after the Jura Mountains, where limestone strata from the period were first identified. The start of the Jurassic was marked by the major Triassic–Jurassic extinction event, associated with the eruption of the Central Atlantic magmatic province, Central Atlantic Magmatic Province. The beginning of the Toarcian Stage started around 183 million years ago and is marked by an extinction event associated with widespread Anoxic event, oceanic anoxia, ocean acidification, and elevated temperatures likely caused by the eruption of the Karoo-Ferrar, Karoo-Ferrar large igneous provinces. The end of the Jurassic, however, has no clear boundary with the Cretaceous and i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Second World War
World War II or the Second World War, often abbreviated as WWII or WW2, was a world war that lasted from 1939 to 1945. It involved the vast majority of the world's countries—including all of the great powers—forming two opposing military alliances: the Allies and the Axis powers. World War II was a total war that directly involved more than 100 million personnel from more than 30 countries. The major participants in the war threw their entire economic, industrial, and scientific capabilities behind the war effort, blurring the distinction between civilian and military resources. Aircraft played a major role in the conflict, enabling the strategic bombing of population centres and deploying the only two nuclear weapons ever used in war. World War II was by far the deadliest conflict in human history; it resulted in 70 to 85 million fatalities, mostly among civilians. Tens of millions died due to genocides (including the Holocaust), starvation, ma ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cambridgeshire
Cambridgeshire (abbreviated Cambs.) is a Counties of England, county in the East of England, bordering Lincolnshire to the north, Norfolk to the north-east, Suffolk to the east, Essex and Hertfordshire to the south, and Bedfordshire and Northamptonshire to the west. The city of Cambridge is the county town. Following the Local Government Act 1972 restructuring, modern Cambridgeshire was formed in 1974 through the amalgamation of two administrative counties: Cambridgeshire and Isle of Ely, comprising the Historic counties of England, historic county of Cambridgeshire (including the Isle of Ely); and Huntingdon and Peterborough, comprising the historic county of Huntingdonshire and the Soke of Peterborough, historically part of Northamptonshire. Cambridgeshire contains most of the region known as Silicon Fen. The county is now divided between Cambridgeshire County Council and Peterborough City Council, which since 1998 has formed a separate Unitary authorities of England, unita ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
West Midlands (region)
The West Midlands is one of nine official regions of England at the ITL 1 statistical regions of England, first level of International Territorial Level for Statistics, statistical purposes. It covers the western half of the area traditionally known as the Midlands (England), Midlands. The region consists of the ceremonial counties of england, counties of Herefordshire, Shropshire, Staffordshire, Warwickshire, West Midlands (county), West Midlands and Worcestershire. The region has seven cities; Birmingham, Coventry, Hereford, Lichfield, Stoke-on-Trent, Wolverhampton and Worcester, England, Worcester. The West Midlands region is geographically diverse, from the urban central areas of the West Midlands conurbation to the rural counties of Herefordshire, Shropshire and Worcestershire which border Wales. The region is landlocked. However, the longest river in the UK, the River Severn, traverses the region southeastwards, flowing through the county towns of Shrewsbury and Worc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Solway Plain
The Solway Plain or Solway Basin is a coastal plain located mostly in northwest Cumbria in England, extending just over the Scottish border to the low-lying area around Gretna and Annan. It lies generally north and west of Carlisle along the Solway Firth, and is drained by the rivers Esk and Lyne. It is associated with the westernmost part of Hadrian's Wall. In medieval times, clay houses known as ''dabbins'' were commonly built on the Solway Plain. The Solway coast has been designated an “Area of Outstanding Natural Beauty”. The plain is known for its archaeological heritage. Archaeological finds that are mentioned in Hodgson and Brennand include urned cremation cemeteries at Ewanrigg, evidence suggesting an ancient domestic settlement at Plasketlands, and evidence suggesting pre-Roman occupation at Ewanrigg, Wolsty Hall and Boustead Hill (among other sites). Salta Moss, where a Bronze Age rapier was discovered, boasts flora that is unusual for a mire on the Solway Plain, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Edenside
Edenside is a cricket ground in Carlisle, Cumbria. The ground is the primary home ground of Cumbria County Cricket Club. The first recorded match on the ground was in 1850, when Carlisle played an All-England Eleven. The ground hosted its first Minor Counties Championship match when Cumberland played the Yorkshire Second XI in 1955. From 1955 to present, the ground has hosted 45 Minor Counties Championship matches. To date the ground has not hosted any MCCA Knockout Trophy matches. The ground has hosted 2 List-A matches, the first of which saw Cumberland play Middlesex in the 1996 NatWest Trophy. The second List-A match played on Edenside saw Cumberland play Kent in the 2000 NatWest Trophy. The home county lost both of these matches against their professional, first-class opponents. In local domestic cricket, Edenside is the home ground of Carlisle Cricket Club. who play in the North Lancashire and Cumbria League Premier Division. Flooding Being situated on the banks of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
