Geomagnetic reversals are events where the Earth's magnetic field changes direction, causing the magnetic north and south poles to switch places. These reversals occur over thousands to millions of years and are recorded in the geological layers of rocks, particularly in oceanic crust. The last major reversal, known as the Brunhes-Matuyama reversal, happened about 780,000 years ago. While the exact cause of these reversals is not fully understood, they are believed to be linked to the movement of molten iron within the Earth's outer core, which generates the planet's magnetic field.