What are the contributions of Charles Lyell?
British lawyer and geologist, one of the founders of modern geology. Lyell was one of the most prominent representatives of uniformitarianism and geological gradualism. His book Principles of Geology, published between 1830 and 1833 in several volumes, is his most outstanding work.
What does Charles Lyell state in his book Principles of Geology?
Principles of Geology (in English: Principles of Geology) is a book written by Scottish geologist Charles Lyell. In it he tried to explain the past changes that the Earth’s surface has experienced, taking into account the causes that are still at work today.
When did uniformitarianism emerge?
From 1830 to 1833, Charles Lyell’s Principles of Geology were published in several volumes. William Whewell coined the terms «uniformitarianism» for this idea and «catastrophism» for the opposite point of view in a review of Lyell’s book.
Who is the father of modern Geology in the principle of the oblique cut?
James Hutton Professional Information Area Geology, Medicine, Chemistry, Naturalism and Experimental Agriculture Known as Father of Modern Geology Plutonism Deep Time Member of Philosophical Society Royal Society of Edinburgh (founder, with others, in 1783) Royal Academy of Agriculture of Paris
Who was James Hutton and what was his contribution to the history of geology?
Physicist and English geologist, born in 1726 in Edinburgh and died in 1797. He developed the theory of uniformitarianism, according to which the geological phenomena that currently operate on Earth have done so throughout its history with the same intensity as in the present.
What is the theory of uniformitarianism?
Uniformitarianism or uniformitarianism, in philosophy of science, is the principle according to which the natural processes that acted in the past are the same that act in the present and with the same intensity.
What is the principle of uniformitarianism?
The geological principle formulated by James Hutton in 1795 and publicized by Charles Lyell in 1830, according to which the geological processes that occur today occurred in a similar way in the past, which is often articulated with the phrase «The present is the key to the past.”