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The Rejection of Continental Drift

Author: Naomi Oreskes
language: en
Publisher: Oxford University Press
Release Date: 1999-04-01
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.
Earth

This book seeks to provide a new and integrated perspective on the Earth. Supporting the earth expansion theory and based on it, the book offers a new interpretation on the total earth system including global tectonics, which explains the cause of earth’s expansion, formation of the continents, oceans and mid-oceanic ridges, formation of mountain ranges, the nature of mantle, core and fluid geosphere, magnetic features of the planet, distribution of temperature pressure and gravity in the interior of the planet, cause of perennial heat of the planet and various other features of global significance. The book offers a totally new concept and interpretation of gravity and provides explanations as to why the earth’s core of the outer core using the new theory and the implication of the earth’s rotation in revamping and shaping the crustal manner.