The attraction of the pyramids: virtual realization of Hutton's suggestion to improve Maskelyne's 1774 Earth density estimate

Charles Hutton suggested in 1821 that the pyramids of Egypt be used to site an experiment to measure the deflection of the vertical by a large mass. The suggestion arose as he had estimated the attraction of a Scottish mountain as part of Nevil Maskelyne's (1774) "Schiehallion Experimen...

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Main Author: J. R. Smallwood
Format: Article
Language:English
Published: Copernicus Publications 2018-01-01
Series:History of Geo- and Space Sciences
Online Access:https://www.hist-geo-space-sci.net/9/1/2018/hgss-9-1-2018.pdf
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spelling doaj-accf393ccd454ee484df5419debd783a2020-11-24T20:59:50ZengCopernicus PublicationsHistory of Geo- and Space Sciences2190-50102190-50292018-01-0191710.5194/hgss-9-1-2018The attraction of the pyramids: virtual realization of Hutton's suggestion to improve Maskelyne's 1774 Earth density estimateJ. R. Smallwood0UCL Hazard Centre, Department of Earth Sciences, UCL, Gower Street, London WC1E 6BT, UKCharles Hutton suggested in 1821 that the pyramids of Egypt be used to site an experiment to measure the deflection of the vertical by a large mass. The suggestion arose as he had estimated the attraction of a Scottish mountain as part of Nevil Maskelyne's (1774) "Schiehallion Experiment", a demonstration of Isaac Newton's law of gravitational attraction and the earliest reasonable quantitative estimate of Earth's mean density. I present a virtual realization of an experiment at the Giza pyramids to investigate how Hutton's concept might have emerged had it been undertaken as he suggested. The attraction of the Great Pyramid would have led to inward north–south deflections of the vertical totalling 1.8 arcsec (0.0005°), and east–west deflections totalling 2.0 arcsec (0.0006°), which although small, would have been within the contemporaneous detectable range, and potentially given, as Hutton wished, a more accurate Earth density measurement than he reported from the Schiehallion experiment.https://www.hist-geo-space-sci.net/9/1/2018/hgss-9-1-2018.pdf
collection DOAJ
language English
format Article
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author J. R. Smallwood
spellingShingle J. R. Smallwood
The attraction of the pyramids: virtual realization of Hutton's suggestion to improve Maskelyne's 1774 Earth density estimate
History of Geo- and Space Sciences
author_facet J. R. Smallwood
author_sort J. R. Smallwood
title The attraction of the pyramids: virtual realization of Hutton's suggestion to improve Maskelyne's 1774 Earth density estimate
title_short The attraction of the pyramids: virtual realization of Hutton's suggestion to improve Maskelyne's 1774 Earth density estimate
title_full The attraction of the pyramids: virtual realization of Hutton's suggestion to improve Maskelyne's 1774 Earth density estimate
title_fullStr The attraction of the pyramids: virtual realization of Hutton's suggestion to improve Maskelyne's 1774 Earth density estimate
title_full_unstemmed The attraction of the pyramids: virtual realization of Hutton's suggestion to improve Maskelyne's 1774 Earth density estimate
title_sort attraction of the pyramids: virtual realization of hutton's suggestion to improve maskelyne's 1774 earth density estimate
publisher Copernicus Publications
series History of Geo- and Space Sciences
issn 2190-5010
2190-5029
publishDate 2018-01-01
description Charles Hutton suggested in 1821 that the pyramids of Egypt be used to site an experiment to measure the deflection of the vertical by a large mass. The suggestion arose as he had estimated the attraction of a Scottish mountain as part of Nevil Maskelyne's (1774) "Schiehallion Experiment", a demonstration of Isaac Newton's law of gravitational attraction and the earliest reasonable quantitative estimate of Earth's mean density. I present a virtual realization of an experiment at the Giza pyramids to investigate how Hutton's concept might have emerged had it been undertaken as he suggested. The attraction of the Great Pyramid would have led to inward north–south deflections of the vertical totalling 1.8 arcsec (0.0005°), and east–west deflections totalling 2.0 arcsec (0.0006°), which although small, would have been within the contemporaneous detectable range, and potentially given, as Hutton wished, a more accurate Earth density measurement than he reported from the Schiehallion experiment.
url https://www.hist-geo-space-sci.net/9/1/2018/hgss-9-1-2018.pdf
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