Showing posts with label Theory. Show all posts
Showing posts with label Theory. Show all posts

Sunday, May 6, 2012

The Rejection of Continental Drift: Theory and Method in American Earth Science For Sale





The Rejection of Continental Drift: Theory and Method in American Earth Science | | Reviews






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The Rejection of Continental Drift: Theory and Method in American Earth Science Reviews





Product Overview


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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Thursday, March 8, 2012

The Rejection of Continental Drift: Theory and Method in American Earth Science For Sale





The Rejection of Continental Drift: Theory and Method in American Earth Science | | Reviews








Product Overview


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.




My Page is a participant in the Amazon Services LLC Associates Program, an affiliate advertising program designed to provide a means for sites to earn advertising fees by advertising and linking to amazon.com

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Wednesday, March 7, 2012

Global Dynamics of the Earth: Applications of Normal Mode Relaxation Theory to Solid-Earth Geophysics (Modern Approaches in Geophysics) For Sale





Global Dynamics of the Earth: Applications of Normal Mode Relaxation Theory to Solid-Earth Geophysics (Modern Approaches in Geophysics) | | Reviews








Product Overview


This volume opens up new perspectives on the physics of the Earth's interior for graduate students and researchers working in the fields of geophysics and geodesy. It looks at our planet in an integrated fashion, linking the physics of its interior to the geophysical and geodetic techniques that record, over a broad spectrum of spatial wavelengths, the ongoing modifications in the shape and gravity field of the planet. Basic issues related to the rheological properties of the Earth's mantle and to its slow deformation will be understood, in both mathematical and physical terms, within the framework of an analytical normal mode relaxation theory. Fundamentals of this theory are developed in the first, tutorial part. The second part deals with a wide range of applications, ranging from changes in the Earth's rotation to post-seismic deformation and sea-level variations induced by post-glacial rebound. In the study of the physics of the Earth's interior, the book bridges the gap between seismology and geodynamics.




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Sunday, February 19, 2012

The Rejection of Continental Drift: Theory and Method in American Earth Science For Sale





The Rejection of Continental Drift: Theory and Method in American Earth Science | | Reviews








Product Overview


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.




My Page is a participant in the Amazon Services LLC Associates Program, an affiliate advertising program designed to provide a means for sites to earn advertising fees by advertising and linking to amazon.com

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Tuesday, February 14, 2012

The Rejection of Continental Drift: Theory and Method in American Earth Science For Sale





The Rejection of Continental Drift: Theory and Method in American Earth Science | | Reviews








Product Overview


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.




My Page is a participant in the Amazon Services LLC Associates Program, an affiliate advertising program designed to provide a means for sites to earn advertising fees by advertising and linking to amazon.com

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Friday, February 3, 2012

Global Dynamics of the Earth: Applications of Normal Mode Relaxation Theory to Solid-Earth Geophysics (Modern Approaches in Geophysics) For Sale





Global Dynamics of the Earth: Applications of Normal Mode Relaxation Theory to Solid-Earth Geophysics (Modern Approaches in Geophysics) | | Reviews








Product Overview


This volume opens up new perspectives on the physics of the Earth's interior for graduate students and researchers working in the fields of geophysics and geodesy. It looks at our planet in an integrated fashion, linking the physics of its interior to the geophysical and geodetic techniques that record, over a broad spectrum of spatial wavelengths, the ongoing modifications in the shape and gravity field of the planet. Basic issues related to the rheological properties of the Earth's mantle and to its slow deformation will be understood, in both mathematical and physical terms, within the framework of an analytical normal mode relaxation theory. Fundamentals of this theory are developed in the first, tutorial part. The second part deals with a wide range of applications, ranging from changes in the Earth's rotation to post-seismic deformation and sea-level variations induced by post-glacial rebound. In the study of the physics of the Earth's interior, the book bridges the gap between seismology and geodynamics.




My Page is a participant in the Amazon Services LLC Associates Program, an affiliate advertising program designed to provide a means for sites to earn advertising fees by advertising and linking to amazon.com

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Saturday, January 7, 2012

Plate Tectonics: An Insider's History Of The Modern Theory Of The Earth For Sale





Plate Tectonics: An Insider's History Of The Modern Theory Of The Earth | | Reviews








Product Overview


Can anyone today imagine the earth without its puzzle-piece construction of plate tectonics? The very term, "plate tectonics," coined only thirty-five years ago, is now part of the vernacular, part of everyone's understanding of the way the earth works.The theory, research, data collection, and analysis that came together in 1967 to constitute plate tectonics is one of the great scientific breakthroughs of the 20th century. Scholarly books have been written about tectonics, but none by the key scientists-players themselves. In Plate Tectonics, editor Naomi Oreskes has assembled those scientists who played key roles in developing the theory to tell - for the first time, and in their own words - the stories of their involvement in the extraordinary evolution of the theory.The book opens with an overview of the history of plate tectonics, including in-context definitions of the key terms that are discussed throughout the book. Oreskes explains how the forerunners of the theory, Wegener and du Toit, inspired how scientists working at the key academic institutions - Cambridge and Princeton Universities, Columbia University's Lamont Doherty Geological Observatory, and the University of California-San Diego's Scripps Institute of Oceanography – competed and collaborated until the theory coalesced in 1967.





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