For more than four centuries, Earth’s magnetic north pole drifted slowly from the Canadian Arctic toward Siberia. In recent decades, that movement has accelerated sharply, surprising scientists who closely monitor the planet’s magnetic behavior and internal dynamics.
Researchers attribute the shift to changes deep within Earth’s outer core, where flowing molten iron generates the magnetic field. Alterations in these powerful currents, especially beneath Siberia, are pulling the magnetic pole at unprecedented speeds compared to the past.
This rapid motion has real-world consequences. Compasses, navigation systems, airport runway alignments, satellites, and even animal migration depend on accurate magnetic data. To keep technology functioning correctly, scientists must frequently update global magnetic models as the pole continues its journey.































