Unpublished paper, 'On the straining of Earth due to secular cooling' by Charles Davison
Reference number: AP/70/4
Date: 1894
Description
Davison writes: 'If the coefficient of dilatation (e) and the conductivity (k) are constant at every point within the earth, and if the temperature (V) was initially the same throughout, the depth of the surface of zero strain after 100 million years is 2.17 miles, the total volume of the crust folded and crushed above that surface is about 184,500 cubic miles, and the mean thickness of the crushed rock spread over the whole surface of the earth is 4.95 ft. (taking e = 0.0000057, k = 400, V = 7000° F .). The smallness of these figures has been claimed by some geologists as a new and strong argument against the contraction theory of mountain evolution.'
Includes two graphs relating to the depth of surface of zero strain over time.
Subject: Mathematics / Physics / Chemistry
Received 10 January 1894. Read 15 February 1894. Communicated by [John Henry] Poynting.
Whilst the Royal Society declined to publish this paper in full, an abstract of the paper was published in volume 55 of the Proceedings of the Royal Society as 'On the straining of the Earth resulting from secular cooling'.
A version of this paper was published in Davison in The London, Edinburgh, and Dublin Philosophical Magazine and Journal of Science: Davison, Charles. 'On the straining of the earth resulting from secular cooling.' The London, Edinburgh, and Dublin Philosophical Magazine and Journal of Science, volume 41, number 249 (1896), pp. 133-138.
- Reference number
- AP/70/4
- Earliest possible date
- 1894
- Physical description
- Ink on paper
- Page extent
- 13 pages
- Format
- Manuscript
Creator name
Charles Davison
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Citation
Charles Davison, Unpublished paper, 'On the straining of Earth due to secular cooling' by Charles Davison, 1894, AP/70/4, The Royal Society Archives, London, https://makingscience.royalsociety.org/items/ap_70_4/unpublished-paper-on-the-straining-of-earth-due-to-secular-cooling-by-charles-davison, accessed on 21 January 2025
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Related Publications
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III. On the straining of the Earth resulting from secular cooling External link, opens in new tab.
Date: 31st December 1894
DOI: 10.1098/rspl.1894.0025
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VIII. Note on Mr. Davison’s paper on the straining of the Earth's crust in cooling External link, opens in new tab.
Date: 31st December 1887
DOI: 10.1098/rsta.1887.0008
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VII. On the distribution of strain in the Earth's crust resulting from secular cooling; with special reference to the growth of continents and the formation of mountain chains External link, opens in new tab.
Date: 31st December 1887
DOI: 10.1098/rsta.1887.0007
Related Records
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Referee's report by William Thomson, Lord Kelvin, on a paper 'On the straining of the Earth resulting from secular cooling' by Charles Davison
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Second letter from William Thomson, Lord Kelvin, to George Howard Darwin, regarding a paper 'On the straining of the Earth resulting from secular cooling' by Charles Davison
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Referee's report by George Howard Darwin, on a paper 'On the straining of the Earth resulting from secular cooling' by Charles Davison
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Letter from George Howard Darwin, to John William Strutt, 3rd Baron Rayleigh, regarding a paper 'On the straining of the Earth resulting from secular cooling' by Charles Davison
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Second letter from George Howard Darwin, to John William Strutt, Lord Rayleigh, regarding a paper 'On the straining of the Earth resulting from secular cooling' by Charles Davison
Creator: George Howard Darwin Reference number: RR/12/79
Hierarchy
This item is part of:
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Archived papers: volume 70, scientific papers submitted the Royal Society unpublished or abstracted, 1891-1894
1891-1894 Reference number: AP/70
Related Fellows
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John Henry Poynting
Communicator
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Archived Papers
Dates: 1768-1989
The 'Archived Papers' collection is comprised of original manuscript scientific papers and letters submitted to the Royal Society which remained unpublished or were abstracted in the journal 'Proceedings of the Royal Society' published from 1830 onwards.View collection