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Hopkinsʼ Plate 6. The upper drawing is a vertical section, and the lower drawing is the same, but cut horizontally. In Hopkinsʼ drawings, the massive coarse-grained Granite is progressively transformed from south to north; first to coarse-grained Gneiss with oriented minerals, and then to finer grained and more micaceous Schist. In modern geology we know that such changes can take place, but not in a south-to-north transition. From Hopkins (1844).
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Textbooks teach the principles of science. Lyellʼs geology textbooks emphasized vertical crustal movement. He avoided far-fetched continental-drift hypotheses by Hopkins in 1844 and Pepper in 1861. Their notions of drift were supported by fossil and paleoclimate evidence, but their causes were global magnetism and electrochemical crystallization an...
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... shale. In some places (as e.g. near Purgono) the matrix is a dark-green silt, without any admixture of sand, but full of boulders of all sizes. Occasionally it is very fine in grain and sometimes assumes a shaley structure. A good instance of this, and one in which the boulder bed is seen resting on the gneiss, is shown in the accompanying Sketch (Fig. 4). [Fig. 19.] of a nullah section near the village of Kandusa on the Northern boundary of the field. The question naturally, indeed inevitably, suggests itself-How these enormous blocks of stone, manifestly requiring a great force to abrade and transport them, are found mixed with a sediment so fine, that in any, except a very sluggish ...
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... and, so far as known, the animals were of the same kinds as those of America. From this and other evidence it appears that the great northern continent Eria (Fig. 434) was still intact and was the land across which the plants and animals of Triassic time readily migrated to and fro. Crocodile-like reptiles of the sprawling type (Mystriosuchus, Fig. 458) and other active forms (Aëtosaurus, Pl. 31, Fig. 9) were common. Genuine turtles occur in the Triassic rocks, showing the group originated in the Permian. No lizards, snakes, or birds are as yet known in rocks of this ...
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... it has still not been translated to English. It had ten maps showing the positions of continents, climate indicators, and climate belts at different geological times. The maps were translated to English and published by Van der Gracht in 1928 (see p. 138). Köppen and Wegenerʼs first map, of modern climate belt and desert locations, is shown here (Fig. 40). The tropics are characterized by warm seas, abundant rainfall, and jungles. Note that desert sands and arid regions (dotted areas) are not found along the Equator, but in belts to the north and south of the tropics. This modern climate zoning must be understood before one can interpret the ancient climate zones. The simplest ...
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... paper had few sketch maps and geologic profiles, but they were intriguing. One map showed the close fit of continents in Gondwana, and the huge area of shallow marine sediments that would be shortened and compressed to form the Himalayas (Fig. 43, area c). And the profiles showed how mountain ranges formed by continental collisions (Fig. 44). But his paper must have been a disappointment. For some reason, his large colored map was not included and was totally unavailable to readers. This publication consisted largely of discussion of the rock patterns and the various folds of an unavailable ...
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... reproduced Wegenerʼs three globe maps as his Figure 163, and made very favorable comments. In a later section, Daly referred again to Wegenerʼs three maps, and followed them up with maps of his own, of the Atlantic (see Fig. 45) and the Pacific ...
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... geological time these have been regions of tension, not of horizontal compression. On the other hand, the Pacific should be, and is, well framed in mountain chains. In brief, the Atlantic and Pacific types of coast-line, fundamental features of the earth, are adequately explained by the hypothesis of the migration of continents. Figure 169 [ Fig. 45] is a map of the Atlantic basin with its great gulflike extension, the Arctic basin. The Circum-Pacific mountains of America are shown in solid black and are marked with the letter P. The east-west, older Hercynian-Appalachian system of the northern hemisphere is in part shown at I by axial lines. The slightly younger east-west system ...
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... involved in the formation of fold mountain belts. Glassy basalt, in solid form but without crystalline structure, would be quite ductile at high temperature. The lower parts of the crust could be removed as they plunge down into this ductile material, as the sediments and the upper part of the crust were folded and horizontally compressed (Fig. 46). The idea resembles subduction and formation of a melange of scraped-off sediments. We now know that the substrate is not basalt or basaltic glass, as Daly envisioned, but ultramafic rocks of the mantle. Although his working hypotheses were not completely correct, they were useful. They could have been improved, but no other North ...
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... on the other hand, the two land-masses are pictured as having been moved closer together, as in figure 7 [Fig. 47], a great number of observations and deductions are now found to be brought into apparent harmony, and these possible "coincidences" are disposed of in the simplest ...
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... volume was published in March 1928, 15 months after the symposium. The title of the book firmly established the phrase continental drift, rather than continental displacement. The North American authors were so critical of this theory that readers now considered it dead. The title page could have served as its tombstone (Fig. 48): Figure 48. The title page of the AAPG book that firmly established the term "continental drift." In the opinions of most North American geologists, it also laid this theory to rest. From Van der Gracht ...
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... North American authors were so critical of this theory that readers now considered it dead. The title page could have served as its tombstone (Fig. 48): Figure 48. The title page of the AAPG book that firmly established the term "continental drift." ...
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... this statement, Longwell used three printed pages, including two large and vacuous map figures (Fig. 49), to show that Australia could be forced-fit in the Arabian Sea between Africa and India. There is no geological matching of the African-Australian-Indian landmasses once they are fit together: Longwell 1928, p. ...
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... first important point Longwell made was that mountain belts are the result of horizontal compression. To illustrate this, he showed a laboratory experiment performed by Bailey Willis (Fig. 54). Longwell described some of the evidence that horizontal compression was the main force in the building of the Alps and other fold mountain ranges: Longwell 1929Longwell , p. 398-400 (also 1932Longwell p.398-399 / also ...
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... The maps were obviously outdated. They had few bathymetric contours and did not show the depth-sounding data that the contours were based upon. His detailed map of the Atlantic between Africa and South America had barely enough bathymetric detail to show the Mid-Atlantic Ridge. Dalyʼs modest map of the Atlantic Ocean from his 1926-book (see Fig. 45) had more detail. Willis may have been satisfied with his outdated maps, but the journal editors should not have accepted them in ...
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... to the north of this barrier (Figs. 1032, 1038). The Indian province was distinct from both the others. [Grabauʼs Fig. 1032 was a redrawn version On his paleogeographic maps he showed more information than others had done. He tried to indicate not only the coastlines, but also the locations of highlands, and the flow-directions of ancient rivers (Fig. 74), based on the preserved record of sedimentary deposits and fossils. Grabau's texts General Geology and Historical Geology were written for the same college market that the books by Pirsson and Schuchert were serving. This was stiff competition, and Grabau's books were printed only once. On the other hand, his earlier book Principles of ...
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... clouds were finally gone from the Atlantic coast on all three maps of Late Cretaceous time (Fig. 83). By then, Pangaea had broken up and the Atlantic Ocean had opened. For the three maps of Cenozoic time, no clouds were shown anywhere on the maps (Fig. 84). When Dunbar wrote that the clouds were "a device to hide critical areas" we can understand this as meaning a device to hide the ocean, which did not yet exist east of North America. Dunbar and Schuchert continually tried to hide evidence for mobilism in their writing and their ...
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Terrane accretion is a ubiquitous process of plate tectonics that delivers fragments of subduction-resistant lithosphere into a subduction zone, resulting in events such as ocean plateau docking or continental assembly and orogenesis. The post-collisional extension of continental terranes is a well-documented tectonic process linked with gravitatio...
Citations
... Although it was well researched and presented in a few respectable books by Wegener and other scientists, it was ridiculed by geologists and fossil experts. The strong evidence for it was kept out of geology textbooks and scientific journals for 40 years (Krill 2014). Then continental drift was corroborated by a new type of data-the magnetic record of rocks on the seafloor. ...
The aquatic ape hypothesis for human evolution can account for all the traits that distinguish humans from chimpanzees. This scientific paradigm has been considered impossible. It would require that human ancestors maintained a semiaquatic lifestyle for millions of years, whereas hominin fossils indicate relatively dry terrestrial environments. Here I propose a marine aquatic evolution that is speculative, but compatible with all the fossil and genetic evidence. In this hypothesis, hominins evolved from chimpanzee-like apes that became stranded on proto-Bioko — new volcanic islands with no terrestrial foods available. The apes were forced to eat shellfish and seaweed. From wading in water on two legs to obtain food, their bodies evolved to become bipedal. Naked skin, blubber, and protruding noses were also aquatic adaptations. Brain-size increase resulted from marine fatty acid DHA. Some of these hominins escaped to mainland Africa and their bipedal descendants are recorded at the famous fossil sites. The volcanic islands grew and evolved into Bioko, and the hominins that remained there evolved into Homo sapiens. They gave up their marine diet and semiaquatic habitat after food became available on the evolving island. Then, during one of the low sea-level stands in the Pleistocene epoch, humans walked to the mainland on the emergent Bioko land bridge. Unlike earlier aquatic ape ideas, the Bioko scenario can be tested by DNA. If the human genome includes a retrovirus that is otherwise only found in endemic animals on Bioko, it would show that our ancestors came from there. Unfortunately, Bioko and west-central Africa are not interesting to traditional paleoanthropologists, because they do not contain fossils.
The continental drift controversy has been deeply analysed in terms of rationalist notions, which seem to find there a unique topic to describe the weight of evidence for reaching consensus. In that sense, many authors suggest that Alfred Wegener’s theory of the original supercontinent Pangea and the subsequent continental displacements finally reached a consensus when irrefutable evidence became available. Therefore, rationalist approaches suggest that evidence can be enough by itself to close scientific controversies. In this article I analyse continental drift debates from a different perspective which is based on styles of thought. I’ll argue that continental drift debate took much longer than it was usually recognized with two styles of thought coexisting for hundreds of years. These were fixism and mobilism and they were always confronting their own evidence and interpretations and functioning as general frameworks for the acceptability of a specific theory. Therefore, this text aims to bring much broader sociological elements than usually involved in the analysis of the continental drift theory.