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The Age of the Earth from the Changes in its Temperature and Elastic Properties

Gutenberg, B. (1935) The Age of the Earth from the Changes in its Temperature and Elastic Properties. Science, 82 (2116). p. 52. ISSN 0036-8075. https://resolver.caltech.edu/CaltechAUTHORS:20191115-073133706

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Abstract

The results which have been found concerning the age of rocks determine the time which has elapsed since the crystalline crust of the earth has formed. There is a gap which comprises the time between the formation of the earth and the beginning of the geological history.


Item Type:Article
Related URLs:
URLURL TypeDescription
https://doi.org/10.1126/science.82.2116.52-aDOIArticle
Additional Information:© 1935 American Association for the Advancement of Science.
Other Numbering System:
Other Numbering System NameOther Numbering System ID
Balch Graduate School of the Geological Sciences173
Issue or Number:2116
Record Number:CaltechAUTHORS:20191115-073133706
Persistent URL:https://resolver.caltech.edu/CaltechAUTHORS:20191115-073133706
Official Citation:Age of the Earth from the Changes in its Temperature and Elastic Properties. BY B. GUTENBERG. SCIENCE 19 JUL 1935: 52. https://doi.org/10.1126/science.82.2116.52-a
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:99860
Collection:CaltechAUTHORS
Deposited By: Tony Diaz
Deposited On:15 Nov 2019 15:39
Last Modified:12 Feb 2020 23:45

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