Definition
Between the sixteenth and the end of the eighteenth century, the picture of the earth had changed drastically. Time in the narrative of earth was reversed from cyclic theories involving contingent events to linear theories, concerned with cyclic phenomena. Chronologies became longer, assimilating more and more contingent events. Early modern theories of the earth show a world in constant change with an increasingly older past and even more uncertain future. The story of this “incredible discovery of the own history of Earth before, and without, the human one” (Rudwick 2014) is sketched, highlighting the question of the nature of time, the distinction between the formation and the history of earth, the role the legacy of historical narratives played in the birth of stratigraphy (Rappaport 1997), the issue of “slicing history into periods of time” (Le Goff 2014), and finally the first experimental results of the age of the earth.
Introduction
Geology is today generally...
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Acknowledgments
The financial support is provided by Horizon 2020, grant agreement Marie Skłodowska-Curie n°665850. I’d like to thank Mohammadreza Bahrami Hessari (Tehran, Iran) and Azadeh Radbooei (Montreal, Canada) for their kind advice about this chapter. All opinions are mine.
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Chabout-Combaz, B. (2020). Age of the Earth, The. In: Jalobeanu, D., Wolfe, C.T. (eds) Encyclopedia of Early Modern Philosophy and the Sciences. Springer, Cham. https://doi.org/10.1007/978-3-319-20791-9_183-1
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