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A global consortium of scientists has disclosed fresh perspectives on the Moon’s eventful volcanic history, proposing that its crust could have melted several times shortly after its inception.
The discoveries, published in Nature, suggest that the Moon came into existence around 4.43 to 4.51 billion years ago, yet its crust seems to be at least 80 million years more recent due to vigorous volcanic activity.
This research clarifies long-standing discrepancies regarding the Moon’s age, which had previously differed by hundreds of millions of years among experts.
While the majority of lunar rock specimens indicate a younger age, a select few unique zircon crystals point towards an older origin. The researchers theorize that the Moon’s crust was largely remelted post-formation, permitting only a handful of resilient zircons to endure harsh conditions.
The Moon’s tumultuous journey began with a monumental impact between Earth and a Mars-sized entity, yielding a molten substance that eventually aggregated into the Moon.
Initially shrouded by a massive ocean of molten rock, the Moon gradually cooled and settled into its present orbit, roughly 384,400 kilometers from Earth. In its formative years, the Moon orbited significantly closer to Earth, producing notable tidal forces that heated its interior and sparked volcanic activity.
Professor Dr. Francis Nimmo from the University of California Santa Cruz elaborates that during this era, the Moon’s orbit became increasingly elliptical, resulting in fluctuations in distance and velocity which heightened internal heating. This phenomenon likely stirred the Moon’s interior and caused multiple episodes of crustal melting.
The researchers additionally emphasize how this volcanic activity reset the geological timeline of lunar rocks. As these rocks harbor radioactive isotopes that decay over time, their present composition reflects the last time they were heated, rather than their original formation date.
Only a few heat-resistant zircons provide insights into the Moon’s earlier narrative.
These revelations not only illuminate the Moon’s geological chronology but also address earlier mysteries, such as the relatively scarce number of craters on its surface. The team concludes that volcanic activity likely filled ancient impact basins with lava, concealing signs of former collisions.
This study enriches our comprehension of the Moon’s formation and advancement, uncovering a lively history characterized by intense volcanic occurrences that sculpted its current features.
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