You don’t need a telescope to see that the moon is riddled with craters. For billions of years, our celestial neighbor has been absolutely bombarded by asteroids and comets, and the assault has left behind a heavily pockmarked lunar surface.
The largest and oldest-known impact site on the moon is the South Pole-Aitken (SPA) basin, stretching across nearly 1,250 miles (2,000 kilometers) of the far side of the moon. And thanks to new research, scientists have dated the SPA basin to the period between 4.32 and 4.33 billion years ago.
A research team led by scientists at the University of Manchester determined the age of the basin by analyzing a lunar meteorite known as Northwest Africa 2995. The meteorite, which was found in Algeria in 2005, contained uranium and lead that was dated to this period.
So, why is the proposed age of the SPA basin significant? Well, it’s about 120 million years older than expected.
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“For several decades there has been general agreement that the most intense period of impact bombardment was concentrated between 4.2–3.8 billion years ago — in the first half a billion years of the moon’s history,” Joshua Snape, a Royal Society University Research Fellow at The University of Manchester, said in a statement. “But now, constraining the age of the South-Pole Aitken basin to 120 million years earlier weakens the argument for this narrow period of impact bombardment on the moon and instead indicates there was a more gradual process of impacts over a longer period.”
This has implications for Earth’s early history, too. “We know that the Earth and the Moon likely experienced similar impacts during their early history, but rock records from the Earth have been lost,” Romain Tartese, a Senior Lecturer at The University of Manchester, said. “We can use what we have learnt about the moon to provide us with clues about the conditions on Earth during the same period of time.”
While the dating from the Northwest Africa 2995 meteorite has provided a good indication of the SPA basin’s age, the team will have to confirm this data with a sample-return mission from within the crater itself. Good thing we’re going back to the moon!
A paper on the team’s research was published on Oct. 16 in the journal Nature Astronomy.
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