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The fit of the continents around the Atlantic

Bullard, Edward, Everett, J. E., Gilbert Smith, A.·1965·Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences

Abstract

The geometrical fit of the continents now separated by oceans has long been discussed in relation to continental drift. This paper describes fits made by numerical methods, with a ‘least squares’ criterion of fit, for the continents around the Atlantic ocean. The best fit is found to be at the 500 fm. contour which lies on the steep part of the continental edge. The root-mean-square errors for fitting Africa to South America, Greenland to Europe and North America to Greenland and Europe are 30 to 90 km. These fits are thought not to be due to chance, though no reliable statistical criteria are available. The fit of the block assembled from South America and Africa to that formed from Europe, North America and Greenland is much poorer. The root-mean-square misfit is about 130 km. These geometrical fits are regarded as a preliminary to a comparison of the stratigraphy, structures, ages and palaeomagnetic results across the joins.

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Metadata

Authors
Bullard, E., Everett, J. E., & Gilbert Smith, A.
Venue
Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences
Published
1965-10-28
Volume
258
Issue
1088
Pages
41-51
ISSN
  • 0080-4614 (ISSN-L)
  • 2054-0272
OpenAlex
W1964408423
Cited by
1,226
References
0
FWCI
44.68
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: The fit of the continents around the Atlantic. https://app.cochat.ai/papers/10.1098/rsta.1965.0020
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Bullard, E., Everett, J. E., & Gilbert Smith, A. (1965). The fit of the continents around the Atlantic. Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences. https://doi.org/10.1098/rsta.1965.0020

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