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William Pengelly
William Pengelly, Royal Society, FRS Geological Society, FGS (12 January 1812 – 16 March 1894) was a British geologist and amateur archaeologist who was one of the first to contribute proof that the Biblical chronology of the earth calculated by Archbishop James Ussher was incorrect. Biography Born at Looe, East Looe in Cornwall, the son of a sea captain, he left school at the age of 12 to join his father's crew. Returning to Looe while still in his teens, he spent his time reading widely and learning mathematics. In about 1836 he moved to Torquay and opened a day school teaching according to the fashionable Johann Heinrich Pestalozzi, Pestalozzian method. In 1846 he gave up his successful school to become a private tutor and also started lecturing on various scientific subjects – a career he continued for the rest of his life. Pengelly published his first scientific paper in 1849, on fossil fish found in East Cornwall. This was the first of some 120 papers on geology, palae ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Royal Geological Society Of Cornwall
The Royal Geological Society of Cornwall is a geological society based in Penzance, Cornwall in the United Kingdom. It was founded in 1814 to promote the study of the geology of Cornwall, and is the second oldest geological society in the world, after the Geological Society of London which was founded in 1807. History The first President of the society was Davies Gilbert, the first Secretary John Ayrton Paris, and other notable members include Humphry Davy (some of whose papers are held by the Society), and William Gregor, who discovered titanium. The society's first premises was a house in North Parade, Penzance and in 1853 the Borough of Penzance put forward plans for a new public building on the west side of Penzance. It was planned to have the Borough offices, county court and police station in the east wing, the two floors of the west wing housing the RGSC's museum and a public hall between the two run by a public company. The foundation stone was laid on 27 April 1864, th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
John Lee (astronomer)
John Lee LL.D, FRS (28 April 1783 – 25 February 1866), born John Fiott, was an English philanthropist, astronomer, mathematician, antiquarian, barrister, and numismatist. Family He was the eldest son of John Fiott and Harriet, daughter of William Lee, of Totteridge, MP for Appleby, of the family of the Lee baronets of Hartwell. His father was involved in the family counting house business and was a failed East India merchant. He was orphaned when young and was brought up by his maternal uncle, William Lee Antonie. Education Lee read Mathematics at St John's College, Cambridge between 1802 and 1806, graduating fifth wrangler in his year. He was elected a fellow in 1808. Following his studies from 1807–1815 he travelled extensively in the Middle East and Europe as a travelling bachelor. During this time he gained an interest in antiquities. Personal life He took the name Lee in 1816 following the death of his uncle William Lee Antonie in 1815. In 1833 Lee married Cecilia ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Charles Babbage
Charles Babbage (; 26 December 1791 – 18 October 1871) was an English polymath. A mathematician, philosopher, inventor and mechanical engineer, Babbage originated the concept of a digital programmable computer. Babbage is considered by some to be " father of the computer". Babbage is credited with inventing the first mechanical computer, the Difference Engine, that eventually led to more complex electronic designs, though all the essential ideas of modern computers are to be found in Babbage's Analytical Engine, programmed using a principle openly borrowed from the Jacquard loom. Babbage had a broad range of interests in addition to his work on computers covered in his book ''Economy of Manufactures and Machinery''. His varied work in other fields has led him to be described as "pre-eminent" among the many polymaths of his century. Babbage, who died before the complete successful engineering of many of his designs, including his Difference Engine and Analytical Eng ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Royal Society
The Royal Society, formally The Royal Society of London for Improving Natural Knowledge, is a learned society and the United Kingdom's national academy of sciences. The society fulfils a number of roles: promoting science and its benefits, recognising excellence in science, supporting outstanding science, providing scientific advice for policy, education and public engagement and fostering international and global co-operation. Founded on 28 November 1660, it was granted a royal charter by King Charles II as The Royal Society and is the oldest continuously existing scientific academy in the world. The society is governed by its Council, which is chaired by the Society's President, according to a set of statutes and standing orders. The members of Council and the President are elected from and by its Fellows, the basic members of the society, who are themselves elected by existing Fellows. , there are about 1,700 fellows, allowed to use the postnominal title FRS (Fellow of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jacques Boucher De Crèvecœur De Perthes
Jacques Boucher de Crèvecœur de Perthes (; 10 September 1788 – 5 August 1868), sometimes referred to as Boucher de Perthes ( ), was a French archaeologist and antiquary notable for his discovery, in about 1830, of flint tools in the gravels of the Somme valley. Life Born at Rethel, in the Ardennes, he was the eldest son of Jules Armand Guillaume Boucher de Crèvecœur, botanist and customs officer, and of Etienne-Jeanne-Marie de Perthes (whose surname he was authorised by royal decree in 1818 to assume in addition to his father's). In 1802 he entered government employ as an officer of customs. His duties kept him for six years in Italy, but upon his returning in 1811 he found rapid promotion at home, and finally was appointed, in March 1825, to succeed his father as director of the douane (customs office) at Abbeville, where he remained for the rest of his life. Boucher de Perthes as an archaeologist His leisure time was chiefly devoted to the study of what was afterwards c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
John Evans (archaeologist)
Sir John Evans (17 November 1823 – 31 May 1908) was an English archaeologist and geologist. Biography John Evans, son of the Rev. A. B. Evans, was born at Britwell Court, Buckinghamshire. At the age of seventeen he started to work for the paper-manufacturing business of John Dickinson & Co. Ltd at Nash Mills (Hemel Hempstead, Hertfordshire). The company had been founded by his uncle and later father-in-law John Dickinson (1782–1869), who was also its senior partner. In 1850 Evans was admitted as a partner in the company and did not retire from active management until 1885. Apart from his managerial work John Evans was also a distinguished antiquary, archaeologist and numismatist. He was president of the following societies and institutions: * The Society of Antiquaries, from 1885 to 1892. * The Royal Numismatic Society, from 1874 to the time of his death. * The Geological Society of London, from 1874 to 1876. * The Anthropological Institute of Great Britain and Ireland, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geological Society Of London
The Geological Society of London, known commonly as the Geological Society, is a learned society based in the United Kingdom. It is the oldest national geological society in the world and the largest in Europe with more than 12,000 Fellows. Fellows are entitled to the postnominal FGS (Fellow of the Geological Society), over 2,000 of whom are Chartered Geologists (CGeol). The Society is a Registered Charity, No. 210161. It is also a member of the Science Council, and is licensed to award Chartered Scientist to qualifying members. The mission of the society is: "Making geologists acquainted with each other, stimulating their zeal, inducing them to adopt one nomenclature, facilitating the communication of new facts and ascertaining what is known in their science and what remains to be discovered". History The Society was founded on 13 November 1807 at the Freemasons' Tavern, Great Queen Street, in the Covent Garden district of London. It was partly the outcome of a previous cl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Windmill Hill Cavern
Windmill Hill Cavern (also called Windmill Hill Cave, the Brixham Cave, Brixham Bone Cavern and Philp's Cave) is a limestone cave system in the town of Brixham, Devon. It was discovered in 1858 and later excavated by a team led by the geologist William Pengelly, who found proof that humans co-existed with extinct British fauna. Discovery Windmill Hill Cavern was a chance discovery in 1858 by builder John Lane Philp, who was searching for a pickaxe that had fallen into a hole in the ground during construction of a house on Mount Pleasant Road in the northwestern part of Windmill Hill and incidentally came across the cave. Upon hearing about Philp's discovery, the Geological Society of London drew up a lease to secure an excavation of the cavern. William Pengelly, a British geologist and paleontologist, was selected to lead the excavation of the cavern, with geologist Hugh Falconer, supervised by Pengelly, outlining the operation plans for the exploration before beginning. Exca ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stratum
In geology and related fields, a stratum ( : strata) is a layer of rock or sediment characterized by certain lithologic properties or attributes that distinguish it from adjacent layers from which it is separated by visible surfaces known as either '' bedding surfaces'' or ''bedding planes''.Salvador, A. ed., 1994. ''International stratigraphic guide: a guide to stratigraphic classification, terminology, and procedure. 2nd ed.'' Boulder, Colorado, The Geological Society of America, Inc., 215 pp. . Prior to the publication of the International Stratigraphic Guide, older publications have defined a stratum as either being either equivalent to a single bed or composed of a number of beds; as a layer greater than 1 cm in thickness and constituting a part of a bed; or a general term that includes both ''bed'' and ''lamina''.Neuendorf, K.K.E., Mehl, Jr., J.P., and Jackson, J.A. , eds., 2005. ''Glossary of Geology'' 5th ed. Alexandria, Virginia, American Geological Institute. 779 pp. . ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Father John MacEnery
John MacEnery (27 November 1796 – 18 February 1841) was a Roman Catholic priest from Limerick, Ireland and early archaeologist who came to Devon as Chaplain to the Cary family at Torre Abbey in 1822. In 1825, 1826 and 1829, he investigated the prehistoric remains at Kent's Cavern in Devon, having been shown the cave by Thomas Northmore. MacEnery concluded that the palaeolithic flint tools he found in the same contexts as the bones of extinct prehistoric mammals meant that early humans and the creatures such as mammoths co-existed. His contemporaries had great difficulty reconciling his findings to their pre- Darwinian, creationist view of the earth's history. 20th century commentators suggest it was the influence of the theologian William Buckland who persuaded MacEnery to doubt the evidence he saw before him, which led to MacEnery never publishing his work. However, Edward Vivian stated that it was simply the expense which caused him to abandon publication.E. Vivian (ed) Caver ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kents Cavern
Kents Cavern is a cave system in Torquay, Devon, England. It is notable for its archaeological and geological features. The cave system is open to the public and has been a geological Site of Special Scientific Interest since 1952 and a Scheduled Ancient Monument since 1957. Prehistory The caverns and passages were formed in the early Pleistocene period by water action, and have been occupied by one of at least eight separate, discontinuous native populations to have inhabited the British Isles. The other key paleolithic sites in the UK are Happisburgh, Pakefield, Boxgrove, Swanscombe, Pontnewydd, Paviland, Creswell Crags and Gough's Cave. Kents Cavern 4 A prehistoric upper jawbone (maxilla) fragment was discovered in the cavern during a 1927 excavation by the Torquay Natural History Society, and named ''Kents Cavern 4.'' The specimen is on display at the Torquay Museum. In 1989 the fragment was radiocarbon dated to 36,400–34,700 years BP, but a 2011 study that dated fossi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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