New measurements of rocks gathered during the Apollo missions indicate that the Moon solidified around 4.43 billion years ago, coinciding with Earth becoming habitable.
The analysis of Moon rocks shows it initially formed as a molten blob post-collision, leading to its layering and the formation of the residual liquid KREEP.
Research on KREEP found in the Apollo rocks suggests it formed around 140 million years after the birth of the Solar System.
Scientists studied the lutetium-hafnium ratio in Moon rocks to determine the timing of KREEP formation, leading to the conclusion of around 4.43 billion years ago.
The Moon's solidification occurred amidst planetary impacts, shedding light on its early history post-formation from a collision with a Mars-sized world.
The study's findings contribute to understanding lunar history and Earth's evolution, with implications for the last major impact on Earth during the Moon's formation.
The dating of lunar cooling aids in comprehending Earth's transformation into a habitable world, crucial for the evolution of life.
By clarifying the Moon's history, scientists are better prepared for upcoming missions like Chang'e and Artemis to gather more lunar knowledge.
Further rock samples from the South Pole-Aitken basin are expected to provide more insights into the Moon's history and geological timeline.
Understanding the Moon's cooling process helps in deciphering the formation of rock deposits like mare basalts, crucial for revealing lunar surface evolution.