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  2. Geomagnetic reversal - Wikipedia

    en.wikipedia.org/wiki/Geomagnetic_reversal

    With the Sun it is observed that the solar magnetic intensity greatly increases during a reversal, whereas reversals on Earth seem to occur during periods of low field strength. [ 41 ] Some scientists, such as Richard A. Muller , think that geomagnetic reversals are not spontaneous processes but rather are triggered by external events that ...

  3. Earth's magnetic field - Wikipedia

    en.wikipedia.org/wiki/Earth's_magnetic_field

    Reversals occur nearly randomly in time, with intervals between reversals ranging from less than 0.1 million years to as much as 50 million years. The most recent geomagnetic reversal, called the Brunhes–Matuyama reversal , occurred about 780,000 years ago.

  4. Magnetic field reversal - Wikipedia

    en.wikipedia.org/wiki/Magnetic_field_reversal

    Gauss-Matuyama reversal, approximately 2.588 million years ago; Jaramillo reversal, approximately one million years ago; Laschamp event, a short reversal that occurred 41,000 years ago; Reversal of the solar magnetic field; Magnetization reversal, a process leading to a 180° reorientation of the magnetization vector with respect to its initial ...

  5. The Earth's magnetic field reverses more often – now ... - AOL

    www.aol.com/news/earth-apos-magnetic-field...

    New research proposes a link between plate tectonics and reversals of the Earth’s magnetic field

  6. Laschamp event - Wikipedia

    en.wikipedia.org/wiki/Laschamp_event

    The Laschamp or Laschamps event was a geomagnetic excursion (a short reversal of the Earth's magnetic field). It occurred between 42,200 and 41,500 years ago, during the end of the Last Glacial Period.

  7. Geomagnetic excursion - Wikipedia

    en.wikipedia.org/wiki/Geomagnetic_excursion

    A geomagnetic excursion, like a geomagnetic reversal, is a significant change in the Earth's magnetic field.Unlike reversals, an excursion is not a long-term re-orientation of the large-scale field, but rather represents a dramatic, typically a (geologically) short-lived change in field intensity, with a variation in pole orientation of up to 45° from the previous position.

  8. Paleomagnetism - Wikipedia

    en.wikipedia.org/wiki/Paleomagnetism

    Magnetostratigraphy uses the polarity reversal history of Earth's magnetic field recorded in rocks to determine the age of those rocks. Reversals have occurred at irregular intervals throughout Earth's history. The age and pattern of these reversals is known from the study of sea floor spreading zones and the dating of volcanic rocks.

  9. Earth’s core might be reversing its spin. It ‘won’t affect ...

    www.aol.com/news/earth-core-might-reversing-spin...

    The gravitational and magnetic forces that factor into the inner core’s movement are likely partly responsible, they said. Importantly, their findings also imply a strong connection between the ...