Recent research suggests that tidal forces reshaped the Moon’s surface, effectively masking its true age.
Analyses of lunar samples collected during NASA’s Apollo missions indicate that the Moon’s crust solidified around 4.35 billion years ago.
Rare lunar zircons—minerals that crystallized at extreme temperatures—suggest the Moon formed as early as 4.5 billion years ago.
Several inconsistencies complicate the timeline of Moon's formation.
A new study suggests that tidal forces caused widespread remelting of the lunar surface around 4.35 billion years ago.
Tidal forces could also account for the scarcity of early impact basins on the Moon’s surface.
The proposed timeline suggests the Moon formed around 4.51 billion years ago.
Deep minerals from the lunar far side can be used to confirm this new theory.
Nailing down the Moon’s precise timeline is crucial for understanding planetary evolution.
With each discovery, our understanding of Earth’s closest neighbor grows deeper, bringing us closer to unraveling the mysteries of the early Solar System.