The process of the reversal of the Earth's magnetic poles is called a magnetic flip. This occurs every 4 or 5 times per million years.
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The Earth magnetic field changes approximately every 200,000 thousand years.
The Earth's magnetic poles move due to changes in the movement of molten iron in the outer core of the Earth. This causes fluctuations in the magnetic field which results in the movement of the magnetic poles.
The magnetic axis is relatively unstable compared to the rotational axis. The magnetic poles move around quite a bit from decade to decade. In fact, geologists have discovered that the alignment of the molecules in some sedimentary materials shows that the north and south magnetic poles actually switch places every few tens of thousands of years.
The sun's magnetic field is complex and dynamic, with both large-scale and small-scale magnetic features. Overall, the sun has a dominant global magnetic field that reverses approximately every 11 years as part of the solar cycle. Additionally, there are smaller-scale magnetic fields present in solar active regions such as sunspots and solar flares.
Earth's magnetic field reverses its polarity irregularly, with north and south magnetic poles switching places every few hundred thousand years. This phenomenon is known as geomagnetic reversal. The last complete reversal happened around 780,000 years ago.