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Encyclopedia > Charles Lapworth

Charles Lapworth (September 20, 1842March 13, 1920) was an English geologist. September 20 is the 263rd day of the year (264th in leap years). ... 1842 was a common year starting on Saturday (see link for calendar). ... March 13 is the 72nd day of the year in the Gregorian calendar (73rd in leap years). ... 1920 is a leap year starting on Thursday (link will take you to calendar) // Events January January 7 - Forces of Russian White admiral Kolchak surrender in Krasnoyarsk. ... Geology (from Greek γη- (ge-, the earth) and λογος (logos, word, reason)) is the science and study of the Earth, its composition, structure, physical properties, history, and the processes that shape it. ...


Born at Faringdon, Berkshire, and trained as a teacher, Lapworth settled in the Scottish border region, where he investigated the previously little-known fossil fauna of the area. He married in 1869 and stayed in the area. Eventually, through patient mapping and innovative use of index fossil analysis, 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. Map sources for Faringdon at grid reference SU2895 Faringdon is a town in Oxfordshire in the United Kingdom. ... For other places named Berkshire, see: Berkshire (disambiguation) Berkshire (IPA: or  ; sometimes abbreviated to Berks) is a county in the south of England, to the west of London and also bordering on Oxfordshire, Buckinghamshire, Greater London, Surrey, Wiltshire and Hampshire. ... Scotland (Alba in Scottish Gaelic) is a country in northwest Europe and a constituent nation of the United Kingdom. ... A fossil Ammonite Fossils are the mineralized remains of animals or plants or other traces such as footprints. ... Fauna is a collective term for animal life. ... 1869 is a common year starting on Friday (link will take you to calendar). ... The Silurian is a major division of the geologic timescale that extends from the end of the Ordovician period, about 439 million years ago (mega years ago, mya), to the beginning of the Devonian period, about 408. ...


Eventually his controversial analysis was accepted, and he slowly rose to become one of the leading geologists in the British Isles. He served as a professor at several colleges, and received numerous awards for his work. He is best known for pioneering faunal analysis of Silurian beds by means of index fossils, and his proposal (eventually adopted) that 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. This proposal resolved a heated argument over the age of the strata in question. The British Isles consist of Great Britain, Ireland and a number of much smaller surrounding islands. ... The Cambrian is a major division of the geologic timescale that begins about 542 million years before the present (BP) at the end of the Proterozoic eon and ended about 490 million years BP with the beginning of the Ordovician period. ... National motto: Cymru am byth (Welsh: Wales for ever) Waless location within the UK Official languages English(100%), Welsh(20. ... The Silurian is a major division of the geologic timescale that extends from the end of the Ordovician period, about 439 million years ago (mega years ago, mya), to the beginning of the Devonian period, about 408. ... The Ordovician period is the second of the six (seven in North America) periods of the Paleozoic era. ...


  Results from FactBites:
 
The  Lapworth Museum (712 words)
Charles Lapworth was born in Faringdon, Berkshire and trained as a school teacher in Oxfordshire, his main interests at that time being literature, history, art and music.
Lapworth recognised the importance of the graptolite fossils within the rocks of the Southern Uplands, and how they could be used to zone and correlate the sequences across the area.
Lapworth was familiar with the latest research of Heim and Suess in the Alps, and realised that the superposition of metamorphosed gneiss and quartzite on top of limestone was due to complex, contractional folding and faulting - in short, it was due to what we would now call thrusting.
Charles Lapworth - Wikipedia, the free encyclopedia (211 words)
Charles Lapworth (September 20, 1842 March 13, 1920) was an English geologist.
Born at Faringdon, Berkshire, and trained as a teacher, Lapworth settled in the Scottish border region, where he investigated the previously little-known fossil fauna of the area.
Eventually, through patient mapping and innovative use of index fossil analysis, 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.
  More results at FactBites »

 

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