Gravity study shows why moon's two sides look so different
An exhaustive examination of lunar gravity using data obtained by two Nasa robotic spacecraft is offering new clues about why the two sides of the moon — the one perpetually facing Earth and the other always facing away — look so different.
The data from the US space agency's Gravity Recovery and Interior Laboratory (GRAIL), mission indicates that the moon's deep interior has an asymmetrical structure, apparently caused by intense volcanism on its nearside billions of years ago that helped shape its surface features.
The researchers discovered that the lunar nearside flexes slightly more than the farside during its elliptical orbit around Earth thanks to our planet's gravitational influence — a process called tidal deformation. This indicates differences in the two sides of the lunar interior, they said, specifically in the geological layer called the mantle.
"Our study shows that the moon's interior is not uniform: the side facing Earth - the nearside — is warmer and more geologically active deep down than the far side," said Ryan Park, supervisor of the Solar System Dynamics Group at Nasa's Jet Propulsion Laboratory in California and lead author of the study published on Wednesday in the journal Nature.
The moon's nearside is covered by vast plains, called mare, formed from molten rock that cooled and solidified billions of years ago. Its far side has much more rugged terrain, with few plains.

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