David Leslie Linton
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David Leslie Linton
David Leslie Linton (12 July 1906 – 11 April 1971) was a British geographer and geomorphologist, was professor of geography at Sheffield and Birmingham, best remembered for his work on the landscape development of south-east England with S. W. Wooldridge, and on the development of tors. Early life and education David Linton was born in 1906 in New Cross, London, the second of three children of parents from northern Ireland. He was educated at the nearby Haberdashers' Aske's Hatcham School and King's College London. He received a first class general honours degree in chemistry, physics, and geology in 1926 and a first class special honours degree in geography in 1927. Academic career On graduation Linton initially worked at King's as demonstrator in geology, taking over from S.W.Wooldridge (later the first professor of geography at King's), who had recently completed his doctorate. In 1929 Linton moved to Edinburgh University. He nevertheless continued to collaborate wit ...
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New Cross
New Cross is an area in south east London, England, south-east of Charing Cross in the London Borough of Lewisham and the SE14 postcode district. New Cross is near St Johns, Telegraph Hill, Nunhead, Peckham, Brockley, Deptford and Greenwich, and home to Goldsmiths, University of London, Haberdashers' Hatcham College and Addey and Stanhope School. New Cross Gate, on the west of New Cross, is named after the New Cross tollgate, established in 1718 by the New Cross Turnpike Trust. It is the location of New Cross station and New Cross Gate station. New Cross Gate corresponds to the manor and district formerly known as Hatcham.Mills, A., ''Dictionary of London Place Names'', (2001), Oxford History The area was originally known as Hatcham (the name persists in the title of the Anglican parishes of St. James, Hatcham along with its school, and All Saints, Hatcham Park). The earliest reference to Hatcham is the Domesday Book of 1086 as ''Hacheham''. It was held by the Bishop of Lis ...
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River Capture
Stream capture, river capture, river piracy or stream piracy is a geomorphological phenomenon occurring when a stream or river drainage system or watershed is diverted from its own bed, and flows instead down the bed of a neighbouring stream. This can happen for several reasons, including: *Tectonic earth movements, where the slope of the land changes, and the stream is tipped out of its former course *Natural damming, such as by a landslide or ice sheet *Erosion, either **Headward erosion of one stream valley upwards into another, or **Lateral erosion of a meander through the higher ground dividing the adjacent streams. **Within an area of karst topography, where streams may ''sink'', or flow underground (a sinking or losing stream) and then reappear in a nearby stream valley *Glacier retreat The additional water flowing down the capturing stream may accelerate erosion and encourage the development of a canyon (gorge). The now-dry valley of the original stream is known a ...
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Richard Chorley
Richard John Chorley (4 September 1927 – 12 May 2002) was an English geographer, and Professor of Geography at Cambridge University, known as leading figure in quantitative geography in the late 20th century, who played an instrumental role in bringing in the use of systems theory to geography. Biography Early education Chorley was born in Minehead, Somerset in an area known as the West Country, with roots in Exmoor and the Vale of Taunton Deane. He was a product of a local primary school and Minehead Grammar School. Later on, Chorley began studying Geomorphology as an undergraduate at the School of Geography at Oxford. He served with the Royal Engineers from 1946 to 1948 and made it Lieutenant. Afterwards he went up to Exeter College, where he obtained his BA with Honours in 1951. Later in 1954 he also obtained his MA at Oxford University, and in 1974 his Sc.D. at Cambridge University. At Oxford he was greatly influenced by R.P. Beckinsale, who advised Chorley to go on ...
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Ralph A
Ralph (pronounced ; or ,) is a male given name of English, Scottish and Irish origin, derived from the Old English ''Rædwulf'' and Radulf, cognate with the Old Norse ''Raðulfr'' (''rað'' "counsel" and ''ulfr'' "wolf"). The most common forms are: * Ralph, the common variant form in English, which takes either of the given pronunciations. * Rafe, variant form which is less common; this spelling is always pronounced , as are all other English spellings without "l". * Raife, a very rare variant. * Raif, a very rare variant. Raif Rackstraw from H.M.S. Pinafore * Ralf, the traditional variant form in Dutch, German, Swedish, and Polish. * Ralfs, the traditional variant form in Latvian. * Raoul, the traditional variant form in French. * Raúl, the traditional variant form in Spanish. * Raul, the traditional variant form in Portuguese and Italian. * Raül, the traditional variant form in Catalan. * Rádhulbh, the traditional variant form in Irish. Given name Middle Ages * Ralp ...
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Queen Elizabeth Hospital, Birmingham
The Queen Elizabeth Hospital Birmingham is a major, 1,215 bed, tertiary NHS and military hospital in the Edgbaston area of Birmingham, situated very close to the University of Birmingham. The hospital, which cost £545 million to construct, opened on 16 June 2010, replacing the previous Queen Elizabeth Hospital and Selly Oak Hospital. It is one of the largest single-site hospitals in the United Kingdom and is part of one of the largest teaching trusts in England. It is named after Queen Elizabeth The Queen Mother, who was queen consort and wife of King George VI from 1936 until his death in 1952. The hospital provides a whole range of services including secondary services for its local population and regional and national services for the people of the West Midlands and beyond. The hospital has the largest solid organ transplantation programme in Europe. It has the largest renal transplant programme in the United Kingdom and it is a national specialist centre for liver, ...
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Geographical Association
The Geographical Association (GA) is an association in the United Kingdom. The organisation aims to improve geographical knowledge of the public through promoting geographical education. It is a registered charity and is independent of state aid. Origins The Geographical Association was formed by five geographers, including Halford John Mackinder, in 1893 as an independent, unincorporated association. The first members got together to use and exchange magic lantern, lantern slides, a leading technology of the day. The history of the first hundred years of the GA was published in 1993 and a more recently a chronological list of key people, events and achievements of the association up to the present day has been produced. The current purpose remains the development of a community of practice for sharing teaching ideas, innovations and understanding about geographical education, but the GA also serves as a voice for and represents the interests of geography teachers in policy and ...
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Institute Of British Geographers
The Royal Geographical Society (with the Institute of British Geographers), often shortened to RGS, is a learned society and professional body for geography based in the United Kingdom. Founded in 1830 for the advancement of geographical sciences, the Society has 16,000 members, with its work reaching the public through publications, research groups and lectures. The Society was founded in 1830 under the name ''Geographical Society of London'' as an institution to promote the 'advancement of geographical science'. It later absorbed the older African Association, which had been founded by Sir Joseph Banks in 1788, as well as the Raleigh Club and the Palestine Association. In 1995 it merged with the Institute of British Geographers, a body for academic geographers, to officially become the Royal Geographical Society ''with IBG''. 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 ...
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British Association For The Advancement Of Science
The British Science Association (BSA) is a charity and learned society founded in 1831 to aid in the promotion and development of science. Until 2009 it was known as the British Association for the Advancement of Science (BA). The current Chief Executive is Katherine Mathieson. The BSA's mission is to get more people engaged in the field of science by coordinating, delivering, and overseeing different projects that are suited to achieve these goals. The BSA "envisions a society in which a diverse group of people can learn and apply the sciences in which they learn." and is managed by a professional staff located at their Head Office in the Wellcome Wolfson Building. The BSA offers a wide variety of activities and events that both recognize and encourage people to be involved in science. These include the British Science Festival, British Science Week, the CREST Awards, Huxley Summit, Media Fellowships Scheme, along with regional and local events. History Foundation The Asso ...
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British Geomorphological Research Group
The ''British Society for Geomorphology'' (BSG), incorporating the British Geomorphological Research Group (BGRG), is the professional organisation for British geomorphologists and provides a community and services for those involved in teaching or research in geomorphology, both in the UK and overseas. The society’s journal, ''Earth Surface Processes and Landforms'' is published by Wiley-Blackwell and online access is available free to members. The society is affiliated with the Royal Geographical Society as an affiliated research group and with the Geological Society of London as a specialist group. Mission The mission of the British Society for Geomorphology is to support scientific excellence in geomorphology through: * fostering excellence and increased investment and support for geomorphology * developing applied geomorphological research, having a major impact on environmental policy and practice and providing a public benefit * disseminating new geomorphological r ...
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Periglacial
Periglaciation (adjective: "periglacial", also referring to places at the edges of glacial areas) describes geomorphic processes that result from seasonal thawing of snow in areas of permafrost, the runoff from which refreezes in ice wedges and other structures. "Periglacial" suggests an environment located on the margin of past glaciers. However, freeze and thaw cycles influence landscapes outside areas of past glaciation. Therefore, periglacial environments are anywhere that freezing and thawing modify the landscape in a significant manner. Tundra is a common ecological community in periglacial areas. History Periglaciation became a distinct subject within the study of geology after Walery Łoziński, a Polish geologist, introduced the term in 1909. Łoziński drew upon the early work of Johan Gunnar Andersson. According to Alfred Jahn, his introduction of his work at the 1910 International Geological Congress held in Stockholm caused significant discussion. In the field trip ...
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Pleistocene
The Pleistocene ( , often referred to as the ''Ice age'') is the geological Epoch (geology), epoch that lasted from about 2,580,000 to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was finally confirmed in 2009 by the International Union of Geological Sciences, the cutoff of the Pleistocene and the preceding Pliocene was regarded as being 1.806 million years Before Present (BP). Publications from earlier years may use either definition of the period. The end of the Pleistocene corresponds with the end of the last glacial period and also with the end of the Paleolithic age used in archaeology. The name is a combination of Ancient Greek grc, label=none, πλεῖστος, pleīstos, most and grc, label=none, καινός, kainós (latinized as ), 'new'. At the end of the preceding Pliocene, the previously isolated North and South American continents were joined by the Isthmus of Panama, causing Great American Interchang ...
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Tertiary
Tertiary ( ) is a widely used but obsolete term for the geologic period from 66 million to 2.6 million years ago. The period began with the demise of the non-avian dinosaurs in the Cretaceous–Paleogene extinction event, at the start of the Cenozoic Era, and extended to the beginning of the Quaternary glaciation at the end of the Pliocene Epoch. The time span covered by the Tertiary has no exact equivalent in the current geologic time system, but it is essentially the merged Paleogene and Neogene periods, which are informally called the Early Tertiary and the Late Tertiary, respectively. The Tertiary established the Antarctic as an icy island continent. Historical use of the term The term Tertiary was first used by Giovanni Arduino during the mid-18th century. He classified geologic time into primitive (or primary), secondary, and tertiary periods based on observations of geology in Northern Italy. Later a fourth period, the Quaternary, was applied. In the early d ...
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