Iron is one of the main elements found in the Earth's inner core, which is characterized by extremely high temperatures and ...

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ESA's Swarm mission, utilizing the faint magnetic signals generated by Earth's ocean tides, offers groundbreaking insights ...

X-ray spectroscopy reveals iron’s structure under extreme conditions Study provides insights into Earth's core melting and phase stability Findings challenge past theories and refine geodynamic models ...

Published in the Proceedings of the National Academy of Sciences, the study found that oxygen-17 isotopes on the moon closely ...

New measurements suggest mysterious continent-sized masses in our planet’s lower mantle may be extremely stable features ...

Scientists released an update to a model that maps the ever-moving pole and has significant implications for navigation ...

Your navigation system just got a critical update, one that happens periodically because Earth’s magnetic north pole keeps moving. Here’s what to know.

Since at least the early 19th century, Earth’s north magnetic pole has been situated in the Canadian Arctic and slowly moving ...

They extend nearly 1000 kilometres up from the outer core into the lower mantle, a slowly-moving layer between Earth’s crust and core. Because seismic waves pass more slowly through these ...

Scientists have captured faint magnetic signatures resulting from the tidal movement of seawater across the planet — and they might have to wait until 2030 to get another shot at it.

Increasingly more “post” than “black,” this album encapsulates the best tenets of Harakiri for the Sky, in pursuit of ...