
Earth’s inner core slows and drifts backward in a 70-year seismic rhythm
Seismic data indicate Earth's solid inner core, long spinning slightly faster than the surface, slowed to match the surface around 2009–2010 and has since fallen behind, effectively drifting backward relative to the rest of the planet. The motion is a relative one (to the mantle) and likely part of a ~70-year oscillation that also influences length of day and the magnetic field; the evidence is indirect and debated, with ongoing work to confirm the oscillation model over the coming decade.













