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  2. File:Magnetic Declination Chart for the International ...

    en.wikipedia.org/wiki/File:Magnetic_Declination...

    File:Magnetic Declination Chart for the International Geomagnetic Reference Field, 2005.pdf. Add languages. Page contents not supported in other languages.

  3. List of geomagnetic reversals - Wikipedia

    en.wikipedia.org/wiki/List_of_geomagnetic_reversals

    The following is a list of geomagnetic reversals, showing the ages of the beginning and end of each period of normal polarity (where the polarity matches the current direction). Source for the last 83 million years: Cande and Kent, 1995. [1] Ages are in million years before present (mya).

  4. Geomagnetic reversal - Wikipedia

    en.wikipedia.org/wiki/Geomagnetic_reversal

    The magnetic field of the Earth, and of other planets that have magnetic fields, is generated by dynamo action in which convection of molten iron in the planetary core generates electric currents which in turn give rise to magnetic fields. [15] In simulations of planetary dynamos, reversals often emerge spontaneously from the underlying dynamics.

  5. File:World Magnetic Declination 2015.pdf - Wikipedia

    en.wikipedia.org/wiki/File:World_Magnetic...

    Original file (5,400 × 3,600 pixels, file size: 1.57 MB, MIME type: application/pdf) This is a file from the Wikimedia Commons . Information from its description page there is shown below.

  6. File:World Magnetic Declination 2010.pdf - Wikipedia

    en.wikipedia.org/wiki/File:World_Magnetic...

    English: This is a world map of magnetic declination created by the National Geophysical Data Center at NOAA. Français : Carte mondiale de la déclinaison magnétique terrestre créé par le centre national des donnée géophysiques ( NGDC ) de l'agence américaine responsable de l'étude de l'océan et de l'atmosphère ( NOAA ).

  7. List of Global Boundary Stratotype Sections and Points

    en.wikipedia.org/wiki/List_of_Global_Boundary...

    Magnetic: Brunhes-Matuyama magnetic reversal. 4] Calabrian: 1.8 Vrica Section, Calabria, Italy Magnetic: Approximately 15 ka after the end of magnetic polarity chronozone C2n (Olduvai). Biologic: Immediately above extinction Discoaster brouweri .

  8. Magnetostratigraphy - Wikipedia

    en.wikipedia.org/wiki/Magnetostratigraphy

    The magnetic property most useful in stratigraphic work is the change in the direction of the remanent magnetization of the rocks, caused by reversals in the polarity of the Earth's magnetic field. The direction of the remnant magnetic polarity recorded in the stratigraphic sequence can be used as the basis for the subdivision of the sequence ...

  9. Chronozone - Wikipedia

    en.wikipedia.org/wiki/Chronozone

    A chronozone or chron is a unit in chronostratigraphy, defined by events such as geomagnetic reversals (magnetozones), or based on the presence of specific fossils (biozone or biochronozone). According to the International Commission on Stratigraphy , the term "chronozone" refers to the rocks formed during a particular time period, while "chron ...