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| | An alternative theory of the origin of the Moon |
 | | The third major competing theory to be developed, was the so-called Co-accretion theory, whereby the Earth and Moon formed in the same region but independently from the same primeval material from which the whole Solar System had formed. |
 | | The theory requires a colossal collision with a massive planet, (the size of Mars), from elsewhere in the Solar System, travelling in an unusual, probably elliptical, orbit which was nevertheless in the plane of the ecliptic, where all the other major planets revolve in closely circular orbits. |
 | | No one can say for sure how long the accretion of the Earth's mantle lasted, but during this period, vast amounts of matter were added to the planet, no doubt on a scale ranging from minute particles to enormous chunks, as judged by the visible craters remaining on planets, natural satellites, and asteroids. |
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