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Caradoc Series

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In geology, Caradoc Series is the name introduced by Roderick Murchison in 1839 for the sandstone series of Caer Caradoc in Shropshire , England . It is the fifth of the six subdivisions (in ascending order) of the Ordovician System, comprising all those rocks deposited worldwide during the Caradocian Age (458 to 448 million years ago).

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37-524: The limits of Murchison's Caradoc series have since been somewhat modified, and through the labours of Charles Lapworth the several members of the series have been precisely defined by means of graptolitic zones. These zones are identical with those found in the rocks of the same age in North Wales, the Bala Series , and the terms Bala or Caradoc series are used interchangeably by geologists when referring to

74-583: A large number of leading independent schools, including public schools such as Radley College . The county has two universities: the ancient University of Oxford and the modern Oxford Brookes University , which are both located in Oxford. In addition, Wroxton College , located in Banbury , is affiliated with Fairleigh Dickinson University of New Jersey . The "dreaming spires" of the University of Oxford are among

111-603: A renowned chemist and Herbert a civil engineer, engineering geologist, stratigrapher and palaeontologist. Lapworth received many awards for his work and contributions to geology. In June 1888 he was elected a Fellow of the Royal Society and in 1891 was awarded their Royal Medal . In 1899, he received the highest award of the Geological Society of London , the Wollaston Medal , in recognition of his outstanding work in

148-710: Is White Horse Hill (261-metre (856 ft)), part of the Berkshire Downs. Oxfordshire was recorded as a county in the early years of the 10th century and lies between the River Thames to the south, the Cotswolds to the west, the Chilterns to the east and the Midlands to the north, with spurs running south to Henley-on-Thames and north to Banbury . Although it had some significance as an area of valuable agricultural land in

185-523: Is due to be completed in January 2023. Oxfordshire Oxfordshire ( / ˈ ɒ k s f ər d ʃ ər , - ʃ ɪər / OKS -fərd-shər, -⁠sheer ; abbreviated Oxon ) is a ceremonial county in South East England . The county is bordered by Northamptonshire and Warwickshire to the north, Buckinghamshire to the east, Berkshire to the south, and Wiltshire and Gloucestershire to

222-468: Is responsible for the most strategic local government functions, including schools, county roads and social services . The county is divided into five local government districts : Oxford , Cherwell , Vale of White Horse (after the Uffington White Horse ), West Oxfordshire and South Oxfordshire , which deal with such matters as town and country planning , waste collection and housing. In

259-649: The 2016 European Union referendum , Oxfordshire was the only English county as a whole to vote to remain in the European Union by a significant margin, at 57.06% (70.27% in the City of Oxford), despite Cherwell (barely) voting to leave at 50.31%. Oxfordshire has a comprehensive education system with 23 independent schools and 35 state secondary schools. Only eight schools do not have a sixth form ; these are mostly in South Oxfordshire and Cherwell districts. Oxfordshire has

296-625: The Caversham area of Reading , now administratively in Berkshire , was historically part of Oxfordshire, as was the parish of Stokenchurch , now administratively in Buckinghamshire . The areas of Oxford city south of the Thames, such as Grandpont , were transferred much earlier, in 1889. Oxfordshire includes parts of three Areas of Outstanding Natural Beauty . In the north-west lie the Cotswolds ; to

333-620: The Hirnant limestone , a thin inconstant bed, which is separated by 1,400 ft (430 m). of slates from the Bala limestone, below this are more slates and volcanic rocks. The latter are represented by large contemporaneous deposits of tuff and felsitic lava which in the Snowdon District are several thousand feet thick. In South Wales the Bala Series contains the following beds in descending order:

370-484: The battle of Blenheim . The gardens, which can be visited, were designed by the landscape gardener "Capability" Brown , who planted the trees in the battle formation of the victorious army. Sir Winston Churchill was born in the palace in 1874. It is open to the public. Chastleton House , on the Gloucestershire and Warwickshire borders, is a great country mansion built on property bought from Robert Catesby , who

407-954: The Carboniferous rocks between Nuneaton and Atherstone, and suggesting a pre-Cambrian date for the Longmyndian rocks that underlay them. He extrapolated these findings to the N.W. Highlands of Scotland, suggesting that the Torridonian sandstone might correspond to the Longmyndian rocks, and thus be pre-Cambrian rather than Cambrian, and that the Durness-Eriboll series, overlaying the Torridonian, would be of Cambrian age rather than Silurian. Again Peach and Horne, surveying in Dundonnell Forest , confirmed Lapworths's suggestion, finding Olenelloid fossils in

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444-602: The Middle Ages and early modern period. The area was part of the Cotswolds wool trade from the 13th century, generating much wealth, particularly in the western portions of the county in the Oxfordshire Cotswolds. Morris Motors was founded in Oxford in 1912, bringing heavy industry to an otherwise agricultural county. The role of agriculture as an employer declined rapidly in the 20th century; currently under one per cent of

481-477: The Midlands and follows the Cherwell from Banbury via Kidlington into the city of Oxford, where these join the navigable Thames. About 15% of the historically named Wilts & Berks Canal , in sporadic sections, has been restored to navigability, including the county-relevant 140 metres near Abingdon-on-Thames where it could, if restored, meet the Thames. Oxfordshire contains a green belt area that fully envelops

518-810: The Southern Uplands Charles Lapworth also devoted time to mapping near Durness in Scotland's northwest highlands and was first to propose the controversial theory that here older rocks were found lying above younger, suggesting complex folding or faulting as a cause. Later Peach and Horne were dispatched to the area and their monumental memoir proved Lapworth correct. In the English Midlands he carried out important work in Shropshire, in particular identifying fossils of Olenelloid trilobites of Cambrian age, demonstrating that Cambrian rocks underlay

555-755: The Southern Uplands while employed as a schoolmaster for 11 years at the Episcopal Church school, Galashiels. He then studied geology and became in 1875 an assistant at Madras College in St Andrews, Fife, and then in 1881 the first professor of geology at Mason Science College , later the University of Birmingham , where he taught until his retirement in 1913. He is best known for pioneering faunal analysis of Silurian beds by means of index fossils , especially graptolites , and his proposal (eventually adopted) that

592-554: The Southern Uplands, and Northwest Highlands of Scotland. There years later, in February 1902, he was elected President of the Geological Society for the years 1902–1904. The glacial Lake Lapworth , was named for him by Leonard Johnston Wills in recognition of his original suggestion of its existence in 1898. Aberdeen University awarded him an honorary doctorate in 1884 and Glasgow University in 1912 (both LLD). In 1916 he

629-723: The Spy Wood group beneath them; these two groups of strata are sometimes spoken of as the Chirbury series. In the Breidden district are the barren Criggeon shales with ashes and flows of andesite. In the Lake district the Coniston limestone series represents the Upper Caradocian, the lower portion being taken up by part of the great Borrowdale volcanic series of rocks. The Coniston limestone series contains

666-646: The Trinucleus seticornis beds (Slade beds, Redhill shales and Sholeshook limestone), the Robeston Wathen beds, and the Dicranograplus shales. The typical graptolites are, in the upper part, Dicellograptus anceps and D. complanatus ; in the lower part, Pleurograptus linearis and Dicranograptus clingani . Meg., 1892; J. B. Marr and T. Roberts, Q. J. G. S., 1885; B. N. Charles Lapworth Charles Lapworth FRS FGS (20 September 1842 – 13 March 1920)

703-979: The Upper and Lower Hartfell series, are recognized in the southern and central area, in Peeblesshire , Ayrshire and Dumfriesshire . In Ireland the Caradoc or Bala series is represented by the limestones of Portraine near Dublin and of the Chair of Kildare; by the Ballymoney series of Wexford and Carnalea shales of County Down . In the Lough Mask district beds of this age are found, as in Wales, interstratified with volcanic lavas and tuffs. Other localities are known in counties Tyrone , Meath and Louth , also in Lambay Island . The Bala Series

740-521: The area. He was headmaster of the school in Galashiels from 1864 to 1875. In 1869 he married Janet, daughter of Galashiels schoolmaster Walter Sanderson. Through mapping and innovative use of index fossil analysis, based on a sequence exposed at Dob's Linn , Lapworth showed that what was thought to be a thick sequence of Silurian rocks was in fact a much thinner series of rocks repeated by faulting and folding. He completed this pioneering research in

777-594: The beds between the Cambrian beds of north Wales and the Silurian beds of South Wales should be assigned to a new geological period: the Ordovician . He resolved the long running " Highlands Controversy . Lapworth received numerous awards for his research work, while for teaching he used the English Midlands as a setting for demonstrating the fieldwork techniques he had pioneered in his own research. Following his researches in

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814-694: The centre of the country, it was largely ignored by the Romans and did not grow in importance until the formation of a settlement at Oxford in the 8th century. Alfred the Great was born across the Thames in Wantage , in the Vale of White Horse. The University of Oxford was founded in 1096, although its collegiate structure did not develop until later on. The university in the county town of Oxford (whose name came from Anglo-Saxon Oxenaford = "ford for oxen ") grew in importance during

851-540: The city in the middle, runs the Thames with its flat floodplains. This river forms the historic limit with Berkshire , remaining so on some lowest reaches. The Thames Path National Trail follows the river from upper estuary to a source. Many smaller rivers in the county feed into the Thames, such as the Thame , Windrush , Evenlode and Cherwell . Some of these have trails running along their valleys. The Oxford Canal links to

888-590: The city of Oxford and extends for some miles to protect surrounding towns and villages from inappropriate development and urban growth. Its border in the east extends to the Buckinghamshire county boundary, while part of its southern border is shared with the North Wessex Downs AONB . It was first drawn up in the 1950s, and all of the county's districts contain some portion of the belt. The Oxfordshire County Council , since 2013 under no overall control ,

925-603: The county south of the River Thames , largely corresponding to the Vale of White Horse district, was historically part of Berkshire . The lowlands in the centre of the county are crossed by the River Thames and its tributaries, the valleys of which are separated by low hills. The south contains parts of the Berkshire Downs and Chiltern Hills , and the north-west includes part of the Cotswolds ; all three regions are Areas of Outstanding Natural Beauty . The county's highest point

962-565: The county's population are involved due to high mechanisation. Nevertheless, Oxfordshire remains a very agricultural county by land use, with a lower population than neighbouring Berkshire and Buckinghamshire, which are both smaller. During most of its history, the county was partitioned as fourteen divisions called hundreds , namely Bampton , Banbury , Binfield , Bloxham , Bullingdon , Chadlington , Dorchester , Ewelme , Langtree , Lewknor , Pyrton , Ploughley , Thame and Wootton . The Oxfordshire and Buckinghamshire Light Infantry ,

999-608: The following subdivisions Ashgill group (Ashgill shales and Staurocephalus limestone) - Rocks of Caradoc age are well developed in southern Scotland; in the Girvan district they have been described as the Ardmillan series with the Drummock group and Barren Flagstone group in the upper portion, and the Whitehouse, Ardwell and Balclatchie groups in the lower part. Similarly, two divisions, known as

1036-736: The fucoid beds of the Durness-Eriboll series. For a modern account and discussion of the elucidation of the geology of the N.W. Highlands, see Oldroyd (1990). He died on 13 March 1920 and is buried in Lodge Hill Cemetery near Birmingham. He married Janet Sanderson in 1869. The couple had five children in total. The first and last born children died during infancy; Ernest, born 22 January 1871 and died 6 February 1871, and Walter Sanderson Lapworth, born in 1882 and died in 1884 before his second birthday. The children who survived to adulthood were Arthur (born c. 1873), Herbert (born c. 1876), and Edith Matilda (born c. 1879). Arthur Lapworth became

1073-615: The main army unit in the area, was based at Cowley Barracks on Bullingdon Green, Cowley . The Vale of White Horse district and parts of the South Oxfordshire administrative district south of the River Thames were historically part of Berkshire , but, in 1974, Abingdon , Didcot , Faringdon , Wallingford and Wantage were added to the administrative county of Oxfordshire under the Local Government Act 1972 . Conversely,

1110-653: The reasons for which Oxford is the sixth most visited city in the United Kingdom by international visitors. Among many notable University buildings are the Sheldonian Theatre , built 1664–68 to the design of Sir Christopher Wren , and the Radcliffe Camera , built 1737–49 to the design of James Gibbs . Blenheim Palace , close to Woodstock , was designed and partly built by the architect John Vanbrugh for John Churchill, 1st Duke of Marlborough , after he had won

1147-592: The south and south-east are the open chalk hills of the North Wessex Downs and the wooded hills of the Chilterns . The north of the county contains the ironstone of the Cherwell uplands. Long-distance walks within the county include the Ridgeway National Trail , Macmillan Way , Oxfordshire Way and the D’Arcy Dalton Way. From the mid-point western edge to the southeast corner of Oxfordshire, via

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1184-600: The uppermost substage of the Ordovician System. The Ordovician rocks of the Caradoc district have been subdivided into the following beds, in descending order: the Trinucleus shales, Acton Scott beds, Longville flags, Chatwell and Soudley sandstones , Harnage shales and Hoar Edge grits and limestone . In the Corndon district in the same county the Caradoc series is represented by the Marrington group of ashes and shales and

1221-402: The west. The city of Oxford is the largest settlement and county town . The county is largely rural, with an area of 2,605 km (1,006 sq mi) and a population of 691,667. After Oxford (162,100), the largest settlements are Banbury (54,355) and Abingdon-on-Thames (37,931). For local government purposes Oxfordshire is a non-metropolitan county with five districts. The part of

1258-619: Was a headteacher and an English geologist who pioneered faunal analysis using index fossils and identified the Ordovician period. Charles Lapworth was born at Faringdon in Berkshire (now Oxfordshire ) the son of James Lapworth. He trained as a teacher at the Culham Diocesan Training College near Abingdon, Oxfordshire. He moved to the Scottish border region, where he investigated the previously little-known fossil fauna of

1295-415: Was described as a group of dark slates and sandstones with beds of limestone which occurs in the neighborhood of Bala, Gwynedd , in north Wales . It was first described by Adam Sedgwick , who considered it to be the upper part of his Cambrian System. The Bala limestone is from 20 to 40 ft (12 m) thick, and is recognizable over most of North Wales. The series in the type area consists of

1332-473: Was elected an Honorary Fellow of the Royal Society of Edinburgh . Papers relating to Charles Lapworth can be found at the University of Birmingham in the Lapworth Museum of Geology , located within the Aston Webb building on the main Edgbaston campus. The Lapworth Archive contains a remarkably complete record of all areas of his research work and teaching. In August 2021 an Archives Revealed funded project began to catalogue and promote Lapworth's archive, which

1369-445: Was one of the men involved in the Gunpowder Plot with Guy Fawkes . Stonor Park , another country mansion, has belonged to the recusant Stonor family for centuries. Mapledurham House is an Elizabethan stately home in the south-east of the county, close to Reading . The Abbey in Sutton Courtenay is a medieval courtyard house . It has been recognised by the Historic Building Council for England (now Historic England ) as

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