The gravitational force between Earth and the Moon primarily governs the phenomenon of tides in Earth's oceans. This gravitational pull causes the water to bulge out on the side of Earth facing the Moon, creating a high tide, while a corresponding high tide occurs on the opposite side due to the centrifugal force of the Earth-Moon system. Additionally, the gravitational interaction also influences the Moon's orbit around Earth, contributing to its phases and the stability of its trajectory.
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