Earth’s Inner Core Is Slowing Down | Seismic Discovery & Magnetic Field Impact Seismic studies reveal that Earth’s solid inner core does not rotate at a constant rate. Since around 2010, it has slowed slightly, lagging behind the mantle and crust. Scientists detected these changes by analyzing tiny differences in seismic wave arrival times through the iron-rich core. This slowdown affects the geodynamo, influencing Earth’s magnetic field and the flow of liquid iron in the outer core. Understandi
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Earth’s inner core actually wobbles like a pendulum 🌍🌀 Recent seismic studies reveal that the solid inner core doesn’t spin at a constant speed — it oscillates back and forth over time, shifting its rotation relative to the rest of the planet. #science #geology #earthscience #research #innovation #TechFactsHub | Factspedia
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