scholarly journals Some Recent Studies of the Pre-History of the Earth's Magnetic Field

1954 ◽  
Vol 6 (4) ◽  
pp. 194-199 ◽  
Author(s):  
J. A. CLEGG ◽  
Mary ALMOND ◽  
P. H. S. STUBBS
2015 ◽  
Vol 26 (1) ◽  
pp. 1
Author(s):  
Doug Morrison ◽  
Ivan Barko

In January 1787, on board Lapérouse's Boussole anchored off Macao, the chevalier de Lamanon wrote a letter to the marquis de Condorcet, the then permanent secretary of the Académie Royale des Sciences in Paris. Lamanon's letter contained a summary of his magnetic observations made up to that point on Lapérouse's famous but ill-fated expedition. The letter, amongst other detail, included evidence that the Earth's magnetic field increased in intensity from the equator towards the poles. Sent to Condorcet via the then minister for the French Navy (the maréchal de Castries), the letter was subsequently lost, but not before it was copied. The copy, with early nineteenth-century ownership identified first to Nicolas Philippe Ledru and subsequently to Louis Isidore Duperrey, was itself then lost for over 150 years, but recently rediscovered bound-in with other manuscripts related to the Lapérouse expedition and terrestrial magnetism, including instructions by Ledru and remarks written in the 1830s and 1840s by Duperrey on Lamanon's letter and observations. The significance of Lamanon's letter and the Ledru and Duperrey manuscripts to the history of geomagnetism is discussed here. Duperrey's notes are transcribed in French for the first time and the Lamanon, Ledru and Duperrey manuscripts are translated into English, also for the first time.


1948 ◽  
Vol 53 (4) ◽  
pp. 349 ◽  
Author(s):  
E. A. Johnson ◽  
Thomas Murphy ◽  
O. W. Torreson

Radiocarbon ◽  
1983 ◽  
Vol 25 (2) ◽  
pp. 229-238 ◽  
Author(s):  
Roy Thompson

The history of the earth's magnetic field is preserved in the fossil magnetism of archaeologic specimens, natural rocks and sediments. Samples such as lava flows and baked sherds that acquired a thermoremanent magnetization on cooling can be used to estimate ancient geomagnetic field intensities and directions. Paleofield directions can also be obtained from fine-grained sediments that acquired detrital magnetic remanence when deposited. Study of the earth's magnetic field over the last few tens of thousands of years yields information on geomagnetic dynamo theories, causes of fluctuations in cosmic-ray activity, and the formulation of a new regional chronologic tool.


2006 ◽  
Vol 246 (1-2) ◽  
pp. 17-26 ◽  
Author(s):  
Y GALLET ◽  
A GENEVEY ◽  
M LEGOFF ◽  
F FLUTEAU ◽  
S ALIESHRAGHI

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