In research published on Monday in the journal Nature Geoscience, these multiple impacts may have created many moons, which eventually coalesced to create The Moon. Therefore, a massive Earth-Theia impact event probably isn't required.
"Our model suggests that the ancient Earth once hosted a series of moons, each one formed from a different collision with the proto-Earth," said Hagai Perets, of the Technion-Israel Institute of Technology, in a statement. "It's likely that such moonlets were later ejected, or collided with the Earth or with each other to form bigger moons."
This alternative scenario assumes that during our planet's formation, it experienced many massive impacts, each kicking debris into orbit that went on to collect under mutual gravity, forming mini-moons or "moonlets." As each new moonlet formed, it settled into orbit and slowly migrated outward. Then, another impact would kick up new debris into orbit, forming another moonlet. These newer moonlets would have a gravitational influence on the older moonlets orbiting further away and their mutual gravity would cause some destabilization. Some moonlets would be flung away, whereas others would fall back to Earth. But others would merge, creating a growing moon that would form the basis of the moon we have today.