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Abū Rayhān al-Bīrūnī publishes the Kitāb fī Taḥqīq mā li-l-Hind, which he discusses the geology of India and hypothesizes that it was once a sea.
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Abraham Ortelius, Flemish-Spanish cartographer, promotes the continental drift theory.
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Nicolas Steno puts forward his theory that sedimentary strata had been deposited in former seas, and that fossils were organic in origin.
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Edmond Halley suggests using evaporation from Mediterranean to determine the age of the Earth.
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James Keir suggests that some rocks, like the ones at the Giant's Causeway, might have been formed by the crystallisation of molten lava.
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Sir Charles Lyell publishes book, Principles of Geology, which describes the world as being several hundred million years old.
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Louis Agassiz begins his glaciation studies which eventually demonstrate that the Earth has had at least one ice age.
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George Darwin and John Joly claim that radioactivity is partially responsible for the Earth's heat.
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Arthur Holmes uses radioactivity to date rocks, the oldest being 1.6 billion years old.
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Physicist Luis Alvarez, and his son Walter Alvarez, and others propose that the impact of a large extraterrestrial object caused the extinction of the dinosaurs at the end of the Cretaceous Period, about 66 million years ago.