Biography of charles lyell
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Charles Lyell
Scottish geologist (1797–1875)
For other people named Charles Lyell, see Charles Lyell (disambiguation).
Sir Charles Lyell, 1st Baronet, FRS (14 November 1797 – 22 February 1875) was a Scottish geologist who demonstrated the power of known natural causes in explaining the earth's history. He is best known today for his association with Charles Darwin and as the author of Principles of Geology (1830–33), which presented to a wide public audience the idea that the earth was shaped by the same natural processes still in operation today, operating at similar intensities. The philosopher William Whewell dubbed this gradualistic view "uniformitarianism" and contrasted it with catastrophism, which had been championed by Georges Cuvier and was better accepted in Europe. The combination of evidence and eloquence in Principles convinced a wide range of readers of the significance of "deep time" for understanding the earth and environment.
Lyell's scientific contributions included a pioneering explanation of climate change, in which shifting boundaries between oceans and continents could be used to explain long-term variations in temperature and rainfall. Lyell also gave influential explanations of earthquakes and developed the theory of gradual "backed up-
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Understanding Evolution
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Catastrophism
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Charles Lyell
Charles Lyell (1797-1875) was a Scottish geologist and Professor of Geology at King’s.
Born on his family’s estate in Scotland, Charles spent much of his childhood in his families second home in Hampshire in the south of England.
He attended Exeter College, Oxford and became a lawyer after graduation. He published his first paper on geology in 1822 and was elected joint secretary of the Geological Society in 1823. In 1827, with his eyesight worsening, he decided to dedicate the rest of his career solely to geology.
Charles is best known for his (literally) ground-breaking Principles of Geology, which propounded the theory of uniformitarianism – the idea that the Earth’s current state is the result of the same forces that are still acting upon it today. The Principlesdemonstrated conclusively that the earth must be millions of years old and opened the way for Charles Darwin’s theories of evolution.
His other scientific contributions included explanations of the causes of earthquakes and the formation of volcanoes and coining the names of the geological eras: Palaeozoic, Mesozoic and Cenozoic.
Charles was knighted in 1848, before inheriting his baronetcy in 1864. He was awarded the Copley Medal of the Royal Society in 1858 and the Wollaston Medal of the