c. 1025 – al-Biruni publishes the Kitāb fī Taḥqīq mā li-l-Hind (Researches on India), in which he discusses the geology of India and hypothesizes that it was once a sea.[1]
1862 – Lord Kelvin attempts to find the age of the Earth by examining its cooling time and estimates that the Earth is between 20 and 400 million years old
1903 – George Darwin and John Joly claim that radioactivity is partially responsible for the Earth's heat
1907 – Bertram Boltwood proposes that the amount of lead in uranium and thorium ores might be used to determine the Earth's age and crudely dates some rocks to have ages between 410 and 2200 million years
1911 – Arthur Holmes uses radioactivity to date rocks, the oldest being 1.6 billion years old
1912 – Alfred Wegener proposes that all the continents once formed a single landmass called Pangaea that broke apart via continental drift
1960 – Harry Hess proposes that new sea floor might be created at mid-ocean rifts and destroyed at deep sea trenches
1963 – Frederick Vine and Drummond Matthews explain the stripes of magnetized rocks with alternating magnetic polarities running parallel to mid-ocean ridges as due to sea floor spreading and the periodic geomagnetic field reversals (Vine–Matthews–Morley hypothesis)
^A. Salam (1984), "Islam and Science". In C. H. Lai (1987), Ideals and Realities: Selected Essays of Abdus Salam, 2nd ed., World Scientific, Singapore, pp. 179–213.
^ abcGarcia-Castellanos, Daniel (27 November 2013). "How old is Earth Science?". Retos Terrícolas. blogspot.com. Retrieved 7 April 2018.
^Alvarez, Walter; Leitão, Henrique (March 2010). "The neglected early history of geology: The Copernican Revolution as a major advance in understanding the Earth". Geology. 38 (3): 231–234. Bibcode:2010Geo....38..231A. doi:10.1130/G30602.1.
^Vai, Gian Battista; Cavazza, William, eds. (2004). Four centuries of the word geology : Ulisse Aldrovandi 1603 in Bologna. Bologna, Italy: Minerva. ISBN9788873810568.