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Geomagnetic Reversal

Geomagnetic reversal is a natural phenomenon where the Earth's magnetic poles switch places, meaning the magnetic north becomes the magnetic south and vice versa. This process occurs irregularly over thousands to millions of years and is recorded in rocks and sediments. Scientists believe it’s linked to changes in the Earth's molten outer core, where magnetic fields are generated. While the exact timing and effects of these reversals are still studied, they do not have immediate consequences for life on Earth; however, they can impact navigation systems and satellites during the transition period.

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    Geomagnetic reversal is a natural phenomenon where Earth's magnetic north and south poles switch places. This process occurs over thousands of years and has happened many times throughout Earth's history. It is caused by changes in the flow of molten iron within the Earth's outer core, which generates our magnetic field. While the reversal itself can disrupt navigation systems and animal migrations temporarily, it is not harmful to life on Earth. Geological records, such as those found in lava flows and ocean sediments, provide evidence of past reversals, helping scientists understand Earth's magnetic history.