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" ... not occur on gentle waves, but in the most compressed flexures of the mountain chains, which in the act of moving have snapped or given way at the summit where the bend is sharpest, the less inclined side being shoved up on the plane of the fault,... "
Proceedings of the American Academy of Arts and Sciences - Página 428
por American Academy of Arts and Sciences - 1883
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Proceedings of the American Academy of Arts and Sciences, Volumen18

American Academy of Arts and Sciences - 1888 - 506 páginas
...side being shoved up on the plane of the fault, this plane being generally parallel to, if it does not coincide with, the axis plane ; and, further,...only. It was based on the observed positions of more than fifty thermal springs in the Appalachian belt, occurring in an area of about fifteen thousand...
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Proceedings of the American Academy of Arts and Sciences, Volumen10

1883 - 524 páginas
...side being shoved up on the plane of the fanlt, this plane being generally parallel to, if it does not coincide with, the axis plane; and, further, that " the direction of these fanlts generally follows the run of the line of elevation of the mountains, the length and vertical...
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Biographical Memoirs

National Academy of Sciences (U.S.) - 1895 - 712 páginas
...side being shoved up on the plane of the fault, this plane being generally parallel to, if it does not coincide with, the axis plane ; and, further,...we referred above was published under the name of Wm. B. Rogers only. It was based on the observed positions of more than fifty thermal springs in the...
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Biographical Memoirs

National Academy of Sciences (U.S.) - 1895 - 472 páginas
...side being shoved up on the plane of the fault, this plane being generally parallel to, if it does not coincide with, the axis plane ; and, further,...the general geological results to which we referred ahove was published under the name of Wrn. B. Rogers only. It was based on the observed positions of...
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Life and Letters of William Barton Rogers, Volumen2

William Barton Rogers, Emma Savage Rogers - 1896 - 490 páginas
...side being shoved up on the plane of the fault, this plane being generally parallel to, if it does not coincide with, the axis plane ; and, further,...depending on the strength of the disturbing force." ' . . . " On the death of the illustrious Henry, he was elected in 1879 President of the National Academy...
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