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The Structure of the Pacific Basin as Indicated by Earthquakes

Gutenberg, B. (1939) The Structure of the Pacific Basin as Indicated by Earthquakes. Science, 90 (2342). pp. 456-458. ISSN 0036-8075. http://resolver.caltech.edu/CaltechAUTHORS:20140804-164748472

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Abstract

Our earth originated about 2,000 million years ago. Great changes must have occurred in its early history, but even yet both gradual and sudden changes show us that it has not gained complete equilibrium. The sudden movements, which we call earthquakes, give us important information about the constitution of the earth.


Item Type:Article
Related URLs:
URLURL TypeDescription
http://www.jstor.org/stable/1666328JSTORArticle
http://dx.doi.org/10.1126/science.90.2342.456DOIArticle
http://www.sciencemag.org/content/90/2342/456PublisherArticle
Additional Information:© 1939 American Association for the Advancement of Science. Abstract of a public address at the Sixth Pacific Congress, Berkeley, Calif., August 1, 1939.
Record Number:CaltechAUTHORS:20140804-164748472
Persistent URL:http://resolver.caltech.edu/CaltechAUTHORS:20140804-164748472
Official Citation:The Structure of the Pacific Basin as Indicated by Earthquakes B. Gutenberg Science, New Series, Vol. 90, No. 2342 (Nov. 17, 1939), pp. 456-458 Published by: American Association for the Advancement of Science Article Stable URL: http://www.jstor.org/stable/1666328
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:47950
Collection:CaltechAUTHORS
Deposited By: George Porter
Deposited On:05 Aug 2014 15:24
Last Modified:13 Feb 2019 18:01

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