The continental drift theory proposed by Alfred Wegener in the early twentieth century was a pivotal advancement in our understanding of the Earth’s geological configuration and its graphical representation. However, already in 1858, the adventurer Antonio Snider-Pellegrini had published La Création et ses Mystères Dévoilés, which included the first-ever depiction of continental drift in two compelling globe maps, drawn by the planetary mapper Charles Bulard, illustrating the Earth’s surface “before” and “after separation.” The first part of this contribution explores the earlier versions of the continental drift hypothesis from the seventeenth to the nineteenth century, identifying the theories and concepts that likely influenced Snider and Bulard’s work. Subsequent sections provide a detailed analysis of their theory, while in the final section, a hitherto unpublished account of Snider’s and Bulard’s lives sheds light on the circumstances and encounters most likely to be relevant to their conceptualization of continental drift. Among these was the presence of the geographer and explorer Alexander von Humboldt. Snider and Bulard’s theory of continental drift is the outcome of a combination of planetary representation, scientific theorization and human exploration, and offers new research perspectives.

Contextualizing the Cartographic Origins of Continental Drift: Antonio Snider-Pellegrini’s La Création et ses Mystères Dévoilés (1858) and Nineteenth-Century Transnational Scientific Networks

Giovanni Modaffari
2025-01-01

Abstract

The continental drift theory proposed by Alfred Wegener in the early twentieth century was a pivotal advancement in our understanding of the Earth’s geological configuration and its graphical representation. However, already in 1858, the adventurer Antonio Snider-Pellegrini had published La Création et ses Mystères Dévoilés, which included the first-ever depiction of continental drift in two compelling globe maps, drawn by the planetary mapper Charles Bulard, illustrating the Earth’s surface “before” and “after separation.” The first part of this contribution explores the earlier versions of the continental drift hypothesis from the seventeenth to the nineteenth century, identifying the theories and concepts that likely influenced Snider and Bulard’s work. Subsequent sections provide a detailed analysis of their theory, while in the final section, a hitherto unpublished account of Snider’s and Bulard’s lives sheds light on the circumstances and encounters most likely to be relevant to their conceptualization of continental drift. Among these was the presence of the geographer and explorer Alexander von Humboldt. Snider and Bulard’s theory of continental drift is the outcome of a combination of planetary representation, scientific theorization and human exploration, and offers new research perspectives.
2025
La théorie de la dérive des continents proposée par Alfred Wegener au début du XXe siècle a constitué une avancée décisive dans notre compréhension de la configuration géologique de la Terre et de sa représentation graphique. Cependant, dès 1858, l’aventurier Antonio Snider-Pellegrini avait publié La Création et ses mystères dévoilés, qui comprenait la toute première représentation de la dérive des continents sur deux cartes mondiales convaincantes, dessinées par le cartographe planétaire Charles Bulard, illustrant la surface de la Terre « avant » et « après la séparation ». La première partie de l’article explore les versions antérieures de l’hypothèse de la dérive des continents du XVIIe au XIXe siècle, en identifiant les théories et les concepts qui ont probablement influencé les travaux de Snider et Bulard. Les sections suivantes fournissent une analyse détaillée de leur théorie, tandis que la dernière section, un récit inédit de la vie de Snider et Bulard, met en lumière les circonstances et les rencontres les plus susceptibles d’avoir influencé leur conceptualisation de la dérive des continents. Parmi celles-ci figurait la présence du géographe et explorateur Alexander von Humboldt. La théorie de la dérive continentale de Snider et Bulard est le résultat d’une combinaison de représentation planétaire, de théorisation scientifique et d’exploration humaine, et offre de nouvelles perspectives de recherche.
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11574/251040
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