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| | chapter 24 |
 | | The retrograde lunar capture orbit contracts due to tidal dissipation until resonance between the lunar orbital period and the spin period of the Earth locks the Moon in a slowly expanding orbit. |
 | | In the latter case it is possible that such material, distributed in the Earth's orbit, caused collisional perturbation of the Moon's precapture orbit, thereby contributing to the capture of the Moon (Kaula and Harris, 1973; Kaula, 1974; Wood and Mittler, 1974; Opik, 1972). |
 | | Subsonic relative velocities, which appear necessary to prevent net loss from the impact crater (Urey and MacDonald, 1971), could thus be achieved both between the Moon and its planetesimals during accretion and between the Moon and normal Earth satellites during the contraction of the capture orbit. |
| history.nasa.gov /SP-345/ch24.htm (300 words) |
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