Bomb#20
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If I'm reading the diagram correctly, the second moon will be four million km away during the period when it's "captured" -- way outside the Hill sphere -- and will complete only a small fraction of a single orbit before it "escapes". I don't think horseshoe orbits are a good analogy for elliptical orbits.The Hill Sphere isn't a hard limit. Beware the werewolves, Earth currently has two moons. The second one will soon be lost, though.We're not going to lose the moon. The earth's Hill sphere is about three times bigger than the orbit the moon will have when it stops moving away, when the earth becomes tidally locked. The lion's share of the earth's original rotational angular momentum has already been transferred to the moon, so it hasn't got all that much further out to go.
(I hope this link behaves--works for me, but it doesn't like it when the board tries to preview it.)
I'm not following. Why would the Earth-Moon system become tidally locked to the Sun? Ignoring red-giant issues, the long-term projection of the three-body system is for the Earth-Moon system to lose angular momentum, with the Moon sinking closer and closer to the Earth, dropping below the Roche Limit, getting ripped apart by tidal forces, and becoming a ring system.Also, remember that there are two systems involved: Sun-Earth and Earth-Moon. Remember, everything locks eventually. Since the Earth-Sun lock is a year then the Earth-Moon lock is also a year--but a year is well outside our Hill Sphere. Given sufficient time the moon is lost.