Earth’s core

E2199089 UNEXPLORED

Earth’s core is the extremely hot, dense central region of our planet, composed mainly of iron and nickel, whose structure and dynamics generate Earth’s magnetic field and influence geologic activity.

Try in SPARQL Jump to: Surface forms Referenced by

All labels observed (1)

Label	Occurrences
Earth’s core canonical	1

Referenced by (1)

Full triples — surface form annotated when it differs from this entity's canonical label.

Adam Dziewonski → researchInterest → Earth’s core ⓘ