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

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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 Subsequent sections provide a detailed analysis of their theory, while in the final section, a hitherto unpublished account of Snider’s and Bulard’s lives sheds light on the circumstances and encounters most likely to be relevant to their conceptualization of continental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.

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  • 10.1093/oso/9780195117325.001.0001
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In the early twentieth century, American earth scientists were united in their opposition to the new--and highly radical--notion of continental drift, even going so far as to label the theory "unscientific." Some fifty years later, however, continental drift was heralded as a major scientific breakthrough and today it is accepted as scientific fact. Why did American geologists reject so adamantly an idea that is now considered a cornerstone of the discipline? And why were their European colleagues receptive to it so much earlier? This book, based on extensive archival research on three continents, provides important new answers while giving the first detailed account of the American geological community in the first half of the century. Challenging previous historical work on this episode, Naomi Oreskes shows that continental drift was not rejected for the lack of a causal mechanism, but because it seemed to conflict with the basic standards of practice in American geology. This account provides a compelling look at how scientific ideas are made and unmade.

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  • 10.1086/378650
Biogeography of Discontinuously Distributed Hydrophytes: A Molecular Appraisal of Intercontinental Disjunctions
  • Nov 1, 2003
  • International Journal of Plant Sciences
  • Donald H Les + 4 more

The extraordinarily wide distributional ranges of aquatic flowering plants have long stimulated phytogeographical discussion. Although aquatic plants occur rarely among the angiosperms, they represent a disproportionately large number of taxa with broad distributions including various intercontinental disjunctions that are manifest even at the species level. Throughout the nineteenth and early twentieth centuries, long‐range dispersal by waterfowl was the prevailing explanation for widespread aquatic plant distributions. This explanation gradually fell into disfavor as biologists raised doubts as to the ability of waterfowl to transport propagules across the extensive transoceanic distances between the continents on which an assortment of aquatic taxa now reside. During the twentieth century, the development of biogeographical displacement theory, i.e., “continental drift,” steadily began to supplant dispersal as the preferred explanation for discontinuous angiosperm distributions. Our study assesses the ...

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  • Geological Society, London, Special Publications
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"Beneath the Earth's dark keel":Tolkien and Geology Gerard Hynes (bio) "O Valar, ye know not all wonders, and many secret things are there beneath the Earth's dark keel" (Lost Tales I 214). So Ulmo explained the Earth's structure to the Valar. It is curious that they, having materially participated in the making of the world, should be uncertain of its form, but Tolkien was himself uncertain how to depict Arda, at this stage (c.1919) and for decades afterwards.1 Henry Gee has rightly observed that it is unsurprising Tolkien was interested in the earth sciences given his own view of his profession: "I am primarily a scientific philologist. My interests were, and remain, largely scientific" (Gee 34; Letters 345). Tolkien, like any educated person of his generation, was exposed to and to a degree internalized both the scientific method and the scientific worldview. For example, in "On Fairy-stories" Tolkien chose to use a geologic metaphor when discussing the preservation of ancient elements in fairy-stories: "Fairy-stories are by no means rocky matrices out of which the fossils cannot be prised except by an expert geologist" (OFS 49). As Verlyn Flieger and Douglas A. Anderson note in their commentary, "The geologic comparison here is both timely and intentional: geology and mythology being coeval disciplines arising in roughly the same period and out of the same human impulse to dig into origins" (OFS 106). The same could, of course, be said of philology. Further, Tolkien was a reader of science fiction and well aware of the expectations it engendered in readers in terms of coherent world building (see Gee 23-41). Given Tolkien's insistence that Middle-earth is our Earth (Letters 220, 239, 283, 376) the inclusion of geological references is part of the "hard recognition that things are so in the world as it appears under the sun" (OFS 65) which is, according to Tolkien, fantasy's essential foundation. But scientific understanding and the theories and discoveries on which it is based develop and change. The importance of scientific developments, and geology in particular, to Tolkien's account of the shaping of Middle-earth has been emphasized by Karen Wynn Fonstad, Alex Lewis and Elizabeth Currie, Henry Gee and Kristine Larsen (Larsen, A Little Earth of His Own, Shadow and Flame).2 The geology Tolkien knew was not static in any way; new discoveries apparently influenced him as he revised his legendarium. The most far-reaching development in geological theory in the twentieth century, though it took most of Tolkien's scholarly lifetime to establish itself, was continental [End Page 21] drift and Tolkien's writing displays an awareness of and receptivity to it.3 Both Robert C. Reynolds and William Sarjeant have offered explanations of the topography of Middle-earth at the end of the Third Age in terms of plate tectonics, but both articles are primarily descriptive and do not address the question of Tolkien's knowledge of geology, particularly the evidence for continental drift developing across the drafts of his legendarium.4 Indications of a growing concern with geological accuracy and a familiarity with continental drift emerge side by side in Tolkien's writings as they developed. Though Tolkien's geology would always have a strong catastrophist element, in the 1930s Tolkien began to incorporate into it a uniformitarian underpinning of geologic time as well as a dynamic theory of geological change. 5 The general uniformitarian consensus in geology in the second half of the nineteenth and opening decades of the twentieth century understandably formed the basis of Tolkien's treatment of geologic time. But the particular form geological change took in his developing presentation of Middle-earth in deep time may be in part the result of Alfred Wegener's then revolutionary theory of continental drift. Briefly put, "continental drift" proposes a lateral movement of land masses across the Earth's surface over geologic time. The notion of continental drift was suggested as early as 1596 in the third edition of Abraham Ortelius' Thesaurus Geographicus where he noticed the symmetry of the African and American coasts and reinterpreted Plato's Critias as referring not to Atlantis sinking but to...

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Traveling Theory: France and the United States by Ieme van der Poel , Sophie Bertho (review)
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Revaews 844 cantend toeclipse thecomplexities ofmonolithic notions of'French' culture and identity. Thisvolume refuses categorically tofall into that trap. Christopher Whyte's consideration ofCorbiere andGoodsir Smith underlines, for instance, theBreton aspectsof theformer's work;MicheleDuclos'sdiscussion ofKenneth White similarly stresses theCeltic dimension ofthepoet'sengagement with francophone culture; andfinally, DavidKinloch, inhisfascinating discussion ofMichel Tremblay inScots translation, describes howtheMontreal-Edinburgh axisofthis transfer reconfigures cultural relations byshort-circuiting Paris andLondon. In Kinloch's version, the'New Alliance'is no longer bi-polar butsubject potentially toa series ofpostcolonial exchanges. 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IemevanderPoel'suseful introduction alludes more MLR,96.3,200I 845 directly toSokal andBricmont, but undermines their claims tonovelty ororiginality. Sheoffiers a more attenuated, comparative account oftheemergence ofcontemporary theory inFrance andtheUSA,whilst focusing oninstitutional andcultural divergences between thetwocountries. The individual essays which follow are deliberately discrete, exploring issues oftransit andcultural specificity from avariety ofperspectives. Thereisno consensus onthenature oftheory's intercontinental travel, with contributors variously describing theFranco-American relationship as 'dialogue', 'appropriation', 'modification', 'enhancement', 'influence', 'importation ',or a morecomplex form of'continental drift', thisfinalnotionsubtly illustrated byChristine vanBoheemen-Saaf, for whom deconstruction 'eventually imported asradically other haditsroots inaspects ofanAnglo-American tradition' (p.56). 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Genesis and Reception of the Continental Drift Hypothesis
  • Nov 25, 2024
  • Indian Science Cruiser
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Today, continental drift is an established truth that was advocated by Alfred Wegener in the year 1912. However, the journey of this theory towards its universal acceptance was not straight forward. In the beginning, it was thought to be merely an alternative to the biblical flood and land bridges to explain parallelism among the continents. There were technological gaps in gathering pieces of evidence in favour of the theory. But as a result of the constant perseverance of a group of truth finders, both in the field and laboratory, from the end of the 1970s, the continental drifting no longer remains a hypothetical proposition but has become an unequivocal reality. Herein, authors have tried to focus on the devotions of those truth-seekers for the continental drifting in brief.

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  • Cite Count Icon 7
  • 10.35767/gscpgbull.19.3.601
Characteristics of Oil Provinces: A Study for Students
  • Sep 1, 1971
  • Bulletin of Canadian Petroleum Geology
  • F K North

Important differences are discernible between oil basins wholly of Tertiary origin (like some Californian basins) and basins of Mesozoic origin nonethless producing from Tertiary rocks (like the Maracaibo basin). Both sets of basins differ in multiple ways from productive Palaeozoic basins. It is suggested that the differences are due primarily to distant migration, which has enabled oil in older sediments to become pooled far out on the forelands, in shelf sediments and non-orogenic traps, whereas Tertiary oils are still in their basins of origin and in traps of orogenic generation. Combinations of Mesozoic and Palaeozoic oil are much rarer than combinations of Mesozoic and Tertiary oil. It is suggested that this has two causes: the spacing of orogenic episodes, which left the first half of Mesozoic time essentially quiescent, and the introduction of a totally new basin-creating mechanism during late Mesozoic time. This involved the creation of extensional basins consequent on continental drift. As oil geologists have been traditionally resistant to the drift hypothesis, it is very likely that there are more new oil provinces still to be found in Mesozoic rocks than in either Tertiary or Palaeozoic. It is also likely that the familiar association between Tertiary oil basins and Tertiary orogenic belts has obscured the fact that the Mesozoic extensional basins opened up by drift continued to be basinal during the early Tertiary; the Gulf Coast is the familiar exemplar. Wherever a large delta was built outwards over the Tertiary breakover between continental and oceanic crust, equally good prospects should be provided. But if the locales are far removed from the Alpine orogenic belts, they will lie well off shorelines defined by the postglacial rise of sea level. The ideal source sediment is deduced to be one that characterizes many oil provinces and is conspicuously rare or absent in other regions -- a dark-coloured, phosphatic pelite or marl, with organic remains almost entirely planktonic or nektonic and almost wholly microscopic except for fish remains.

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