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History of geophysics : ウィキペディア英語版 | History of geophysics
The historical development of geophysics has been motivated by two factors. One of these is the research curiosity of humankind related to Planet Earth and its several components, its events and its problems. The second one is economical usage of Earth resources (ore deposits, petroleum, water resources, etc.) and Earth-related hazards such as earthquakes, volcanoes, tsunamis, tides, and floods. == Classical and observational period ==
In circa 240 BC, Eratosthenes of Cyrene measured the circumference of the Earth, using trigonometry and the angle of the Sun at more than one latitude in Egypt. There is some information about earthquakes in Aristotle's ''Meteorology'', in ''Naturalis Historia'' by Pliny the Elder, and in Strabo's ''Geographica''. Aristotle and Strabo recorded observations on tides. A natural explanation of volcanoes was first undertaken by the Greek philosopher Empedocles (c. 490-430 B.C.), who considered the world divided into four elemental forces: Earth, Air, Fire and Water. Empedocles maintained volcanoes were manifestation of Elemental Fire. Winds and earthquakes would play a key role in explanations of volcanoes. Lucretius, claimed Mount Etna was completely hollow and the fires of the underground driven by a fierce wind circulating near sea level. Observations by Pliny the Elder noted the presence of earthquakes preceded an eruption. Athanasius Kircher (1602–1680) witnessed eruptions of Mount Etna and Stromboli, then visited the crater of Vesuvius and published his view of an Earth with a central fire connected to numerous others caused by the burning of sulfur, bitumen and coal.
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