Geomagnetism denotes to the Earth's magnetic field, which covers from the Earth's interior to where it encounters the solar wind. Generally, it is the field of a massive bar magnet presently tilted about 10 degrees off the Earth's rotational axis. Unlike a bar magnet, the Earth's magnetic field varies over time, as it is produced by a Geodynamo. And, geomagnetic reversals are swings in Earth's magnetic field in which the locations of the magnetic north and south are swapped. In recent times, a reversal has generally happened every 50,000 to 800,000 years, with a usual of 200,000 years. A glut of scientific indication provisions the presence of geomagnetic reverses.

  • Magnetosphere
  • Magnetic and mineralogical studies
  • Thermoremanent magnetization
  • Archeomagnetism
  • Interplanetary magnetic field
  • Geomagnetic field
  • Paleomagnetism

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