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geomagnetic reversal

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geomagnetic reversal

Alternation of the Earth's magnetic polarity. The Earth's internal magnetic field reverses, on average, about every 300,000 to 1 million years. This reversal is very sudden on a geologic time scale, apparently taking about 5,000 years. The time between reversals is highly variable, sometimes less than 40,000 years and at other times as long as 35 million years. No regularities or periodicities have yet been discovered. A long interval of one polarity may be followed by a short interval of opposite polarity. See also polar wandering.


geomagnetic reversal [¦jē·ō·mag¦ned·ik ri′vər·səl]
(geophysics)
Reversed magnetization of the earth's magnetic dipole.


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One sign of this comes from patterns of geomagnetic reversals, when Earth's north and south magnetic poles swap positions.
thesis at the Centre des Faibles Radioactivites at Gif/Yvette by trying to extract information from the magnetization of tiny specimens of sediment, hoping that they would tell him something about geomagnetic reversals.
Their MHD model had produced a geomagnetic reversal entirely on its own, without any provocation from the experimenters.
 
 
 
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