|
Charles Lapworth
Charles Lapworth FRS FGS (20 September 1842 – 13 March 1920) was a headteacher and an English geologist who pioneered faunal analysis using index fossils and identified the Ordovician period. Biography Charles Lapworth was born at Faringdon in Berkshire (now Oxfordshire) the son of James Lapworth. His school in Galashiels in 2021 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 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 resea ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Faringdon
Faringdon is a historic market town in the Vale of White Horse, Oxfordshire, England, south-west of Oxford, north-west of Wantage and east-north-east of Swindon. It extends to the River Thames in the north; the highest ground is on the Ridgeway in the south. Faringdon was Berkshire's westernmost town until the 1974 boundary changes transferred its administration to Oxfordshire. The civil parish is formally known as ''Great Faringdon'', to distinguish it from Little Faringdon in West Oxfordshire. The 2011 Census gave a population of 7,121; it was estimated at 7,992 in 2019. On 1 February 2004, Faringdon became the first place in south-east England to be awarded Fairtrade Town status. History The toponym "Faringdon" means "hill covered in fern". Claims, for example by P. J. Goodrich, that King Edward the Elder (reigned 899–924) died in Faringdon are unfounded. The town was granted a weekly market in 1218, and as a result came to be called Chipping Faringdon. A weekly ou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Madras College
Madras College, often referred to as Madras, is a Scottish comprehensive secondary school located in St Andrews, Fife. It educates over 1,400 pupils aged between 11 and 18 and was founded in 1833 by the Rev. Dr Andrew Bell. History Madras College, founded in 1833, takes its name from the system of education devised by the school's founder, the Rev. Dr Andrew Bell FRSE. However, the origins of the school can be traced to at least the 1490s, through its predecessor institution, the Grammar School of St Andrews. Bell was born in St Andrews in 1753, the son of a local magistrate and wig-maker. He studied at the University of St Andrews where he distinguished himself in mathematics. He became a clergyman of the Church of England and took up an appointment as chaplain to the regiments of the East India Company in Madras (known since 1996 as Chennai), India. One of his duties was to educate the soldiers' children. Because there was a shortage of teachers, he used the older stud ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Longmyndian Supergroup
The Longmyndian Supergroup is a sequence of Late Precambrian rocks that outcrop between the Pontesford–Linley Fault System and the Church Stretton Fault System in the Welsh Borderland Fault System. The supergroup consists of two major geological groups, the Stretton Group and the overlying Wentnor Group. The rocks are a generally regressive sequence from basinal facies to clastic sedimentation. The rocks are thought to be derived from Uriconian mountains that were formed during the southward subduction of an oceanic plate beneath a continental block (ocean closure). The rocks have since been folded due to fault movements and plunge gently to the south. The Longmyndian rocks were deposited in northeast–southwest trending faulted rift basins. These were deposited on top of the Uriconian volcaniclastic deposits. Subsequent ocean closure squeezed these rocks together to provide sub-vertical bedding in the synclinal sequence we see in exposed rocks today. As noted below, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Olenellina
Olenellina is a suborder of the order Redlichiida of trilobites that occurs about halfway during the Lower Cambrian, at the start of the stage called the Atdabanian. The earliest trilobites in the fossil record are arguably Olenellina, although the earliest Redlichiina and Eodiscina follow quickly. The suborder died out when the Lower passed into the Middle Cambrian, at the end of the stage called Toyonian. A feature uniting the Olenellina is the lack of rupture lines (or sutures) in the headshield, which in other trilobites assist the periodic moulting (or ecdysis), associated with arthropod growth. Some derived trilobites have lost facial sutures again (some Eodiscina, all Agnostina, and a few Phacopina), but all of these are blind, while all Olenellina have eyes. Taxonomy The suborder contains four superfamilies: Olenelloidea (with 3 families and 5 stemgroup genera), Judomioidea (with 1 family and 3 stemgroup genera), Nevadioidea, and Fallotaspidoidea (with 3 familie ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
John Horne
John Horne PRSE FRS FRSE FEGS LLD (1 January 1848 – 30 May 1928) was a Scottish geologist. He served as President of the Royal Society of Edinburgh from 1915 to 1919. Life Horne was born on 1 January 1848, in Campsie, Stirlingshire, the son of Janet (''née'' Braid) and James Horne of Newmill, a farmer. He was educated at the High School, Glasgow, and the University of Glasgow where he studied under Lord Kelvin. He left university without graduating at the age on 19. In 1867 he joined the Scottish Branch of HM Geological Survey as an assistant and became an apprentice to Ben Peach. The two soon became good friends and collaborators. Horne was involved in mapping the Central Lowlands. Horne was a logical thinker and writer, complementing Peach's skills of resolving the internal structure of mountains by looking at the surface rocks. Thia approach allowed them to resolve a long-running debate on the "Highlands Controversy" in the 1907 publication of ''The Geological Struct ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ben Peach
Benjamin Neeve Peach (6 September 1842 – 29 January 1926) was a British geologist. Life Peach was born at Gorran Haven in Cornwall on 6 September 1842 to Jemima Mabson and Charles William Peach, an amateur British naturalist and geologist. He was educated at the Royal School of Mines in London and then joined the Geological Survey in 1862 as a geologist, moving to the Scottish branch in 1867. He is best remembered for his work on the Northwest Highlands and Southern Uplands with his friend and colleague John Horne, where they resolved the long-running "Highlands Controversy" with their 1907 publication of ''The Geological Structure of the North-West Highlands of Scotland''. In 1881 he was elected a Fellow of the Royal Society of Edinburgh. His proposers were Archibald Geikie, Sir Charles Wyville Thomson, Peter Guthrie Tait and Robert Gray. He won the Society's Neill Prize for the period 1883–86. He served as the Society's Vice President from 1912 to 1917. He was electe ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Durness
Durness ( gd, Diùranais) is a village and civil parish in the north-west Highlands of Scotland. It lies on the north coast of the country in the traditional county of Sutherland, around north of Inverness. The area is remote, and the parish is huge and sparsely populated, covering an area from east of Loch Eriboll to Cape Wrath, the most north-westerly point of the Scottish mainland. The population is dispersed and includes a number of townships including Kempie, Eriboll, Laid, , Sangobeg, Leirinmore, Smoo, Sangomore, Durine, Balnakeil and Keoldale. Etymology The name could be Norse "Dyrnes", meaning "deer/animal headland". No one knows for sure where the name derives; it has variously been translated as from "Dorainn nis" tempest point, or "Dhu thir nis" the point of the black land; or from the Norse for deerpoint. Or even from the main village "Durine" which would translate as "Dubh Rinn" the black (or fertile) promontory, with the Norse "ness" tacked onto an existing Ga ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lapworth 1891 Olenellus Callavei
Lapworth is a village and civil parish in Warwickshire, England, which had a population of 2,100 according to the 2001 census; this had fallen to 1,828 at the 2011 Census. It lies six miles (10 km) south of Solihull and ten miles (16 km) northwest of Warwick, and incorporates the hamlet of Kingswood. Lapworth boasts a historic church, the Church of St Mary the Virgin, a chapel. Two National Trust sites are nearby: Baddesley Clinton, a medieval moated manor house and garden located in the village of Baddesley Clinton; and Packwood House, a Tudor manor house and yew garden with over 100 trees in Packwood. The church is a building largely of the 13th and 14th centuries. It includes several unusual features: the steeple is connected by a passage to the north aisle and is built sheer with a projecting stair; the clerestory has square-headed windows; and there is a two-storey annex at the west end. In the church the Portland memorial to Florence Bradshaw was the work of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Adam Sedgwick
Adam Sedgwick (; 22 March 1785 – 27 January 1873) was a British geologist and Anglican priest, one of the founders of modern geology. He proposed the Cambrian and Devonian period of the geological timescale. Based on work which he did on Welsh rock strata, he proposed the Cambrian period in 1835, in a joint publication in which Roderick Murchison also proposed the Silurian period. Later in 1840, to resolve what later became known as the Great Devonian Controversy about rocks near the boundary between the Silurian and Carboniferous periods, he and Murchison proposed the Devonian period. Though he had guided the young Charles Darwin in his early study of geology and continued to be on friendly terms, Sedgwick was an opponent of Darwin's theory of evolution by means of natural selection. He strongly opposed the admission of women to the University of Cambridge, in one conversation describing aspiring female students as "nasty forward minxes." Life and career Sedgwick was b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Roderick Murchison
Sir Roderick Impey Murchison, 1st Baronet, (19 February 1792 – 22 October 1871) was a Scotland, Scottish geologist who served as director-general of the British Geological Survey from 1855 until his death in 1871. He is noted for investigating and describing the Silurian, Devonian and Permian systems. Early life and work Murchison was born at Tarradale Castle, Tarradale House, Muir of Ord, Ross-shire, the son of Barbara and Kenneth Murchison. His wealthy father died in 1796, when Roderick was four years old, and he was sent to Durham School three years later, and then the Royal Military College, Great Marlow to be trained for the army. In 1808 he landed with Arthur Wellesley, 1st Duke of Wellington, Wellesley in Portugal, and was present at the actions of Battle of Roliça, Roliça and Battle of Vimeiro, Vimeiro in the Peninsular War as an ensign in the 36th (Herefordshire) Regiment of Foot, 36th Regt of Foot. Subsequently under Sir John Moore (British Army officer), John Mo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Highlands Controversy Of Northwest Scotland
The Highlands controversy was a scientific controversy which started between British geologists in the middle of the nineteenth century concerning the nature of the rock strata in the Northwest Highlands of Scotland. The debate became contentious, even acrimonious, because of some of the personalities involved and because it pitted professional geologists of the Geological Survey against academic and amateur geologists. An initial resolution was achieved by about 1886 but the great complexity and scientific importance of the discovery of the Moine Thrust Belt and the geological processes involved in its creation led to field work continuing for a further twenty years culminating in the 1907 publication by the Geological Survey of a book of fundamental geological significance: ''The Geological Structure of the North-West Highlands of Scotland''. The acrimony was an important factor in the political decision to set up the Wharton Committee of 1899 to review the state-funded Geologi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wales
Wales ( cy, Cymru ) is a Countries of the United Kingdom, country that is part of the United Kingdom. It is bordered by England to the Wales–England border, east, the Irish Sea to the north and west, the Celtic Sea to the south west and the Bristol Channel to the south. It had a population in 2021 of 3,107,500 and has a total area of . Wales has over of coastline and is largely mountainous with its higher peaks in the north and central areas, including Snowdon (), its highest summit. The country lies within the Temperateness, north temperate zone and has a changeable, maritime climate. The capital and largest city is Cardiff. Welsh national identity emerged among the Celtic Britons after the Roman withdrawal from Britain in the 5th century, and Wales was formed as a Kingdom of Wales, kingdom under Gruffydd ap Llywelyn in 1055. Wales is regarded as one of the Celtic nations. The Conquest of Wales by Edward I, conquest of Wales by Edward I of England was completed by 1283, th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
.jpg "Click for more on -> Highlands Controversy Of Northwest Scotland")