Research news on inner core (earth)

The inner core of Earth is the planet’s solid, innermost region, composed primarily of iron with minor nickel and light elements, extending from about 1,220 km radius to the center. It is characterized by extreme pressures (over 330 GPa) and temperatures comparable to the solar surface, yet remains solid due to pressure-induced freezing. Seismic wave studies reveal anisotropy, suggesting preferential crystal alignment, likely of hexagonal close-packed iron. The inner core plays a critical role in geodynamo processes through latent heat release and compositional convection at the inner core boundary, influencing the structure and dynamics of the surrounding liquid outer core.

Measuring iron in motion at Earth-core conditions

It was a journey to the center of the Earth, if only for the briefest of moments. But rather than tunneling thousands of miles from Earth's surface, researchers from Lawrence Livermore National Laboratory (LLNL) and several ...

The hidden chemistry of Earth's core is revealed by how it froze

A study by researchers at the University of Oxford, University of Leeds, and University College London has identified a new constraint on the chemistry of Earth's core, by showing how it was able to crystallize millions of ...

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