Fifty years after the Apollo 11 lunar landing, researchers have found the Moon has a solid core akin to Earth's, shedding light on its composition and evolution.
Published in Nature, the discovery clarifies the presence of iron-rich materials in the Moon's crust, vital for understanding its geological history.
Studies have revealed the Moon features a solid inner core and a fluid outer core, aligning with theories that it possessed a magnetic field in the past.
This breakthrough, confirming the Moon's solid core, concludes decades of speculation and showcases advancements in research.
Identified 20 years ago, the Moon's fluid outer core now has a detected solid inner core of about 500 kilometers, constituting 15% of its total size.
Evidence supports the theory of the Moon differentiating early in history, with heavy materials forming the core and lighter ones the crust.
Researchers used lunar surface data and laser ranging techniques to ascertain the solid core's existence, aiding in understanding the Moon's evolution.
Scientists also observed material movement in the mantle, explaining the presence of iron-rich elements on the lunar surface.
These findings enhance our solar system's history comprehension and shed light on lunar magnetic field disappearance.
The Earth and Moon differ in core size, composition, state, temperature, and magnetic field strength, reflecting their distinct evolutionary paths.