Theory of Continental Drift: A Symposium on the Origin and Movement of Land Masses Both Inter-Continental and Intra-Continental, as Proposed by Alfred Wegener
This publication was written in 1926 during an era of heated discussions on continental drift based on an AAPG Symposium of the same topic. The problem of continental drift raised considerable and spirited discussion in geological circles. Many authorities advocated it; others were undecided but favorably inclined; still others did not favor it, and some of those were violently opposed. The mere possibility of continental drift was firmly denied by some during this era. It was not possible to settle the problem, or even to discuss it thoroughly in a single publication, but the main principles of the theory of drift are covered as are the main theories of the time, offering an intriguing glimpse into the history of geologic approaches to continental drift.
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David White, 1928. "Discussion of Floating Continents", Theory of Continental Drift: A Symposium on the Origin and Movement of Land Masses Both Inter-Continental and Intra-Continental, as Proposed by Alfred Wegener, W. A. J. M. van Waterschoot van der Gracht, Bailey Willis, Rollin T. Chamberlin, John Joly, G. A. F. Molengraaff, J. W. Gregory, Alfred Wegener, Charles Schuchert, Chester R. Longwell, Frank Bursley Taylor, William Bowie, David White, Joseph T. Singewald, Jr., Edward W. Berry
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Abstract
The Köppen-Wegener maps showing continental aggregates and climatic data throughout geological time, though clever, are open to serious criticism. If the continents could drift apart in geologically late time why did they not break up in earlier eras during greater diastrophic revolutions? Geologists should not forget the principle of isostasy.