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  • Giant-Impact Hypothesis: The Leading Theory of Moon Formation
    The Giant-Impact Hypothesis is the dominant theory for the origin of the Moon.

    Here's a summary of the theory:

    * Early Earth Collision: In the early solar system, a Mars-sized object (sometimes called Theia) collided with the young Earth.

    * Debris Cloud: The impact threw a vast amount of Earth's mantle and the impactor's material into orbit around Earth.

    * Moon Formation: This debris cloud coalesced over time through gravitational attraction, forming the Moon.

    Evidence supporting the theory:

    * Lunar Composition: The Moon's composition is remarkably similar to Earth's mantle, but with slightly different isotopic ratios. This suggests that the Moon was formed from a mixture of Earth and the impactor.

    * Angular Momentum: The Earth-Moon system has a surprisingly high angular momentum, which is best explained by the collision.

    * Lunar Orbit: The Moon's orbit is tilted relative to Earth's equator, a characteristic that supports the theory of a large, off-center impact.

    * Computer simulations: Computer models accurately simulate the formation of the Moon from a giant impact, including the Moon's size, composition, and orbit.

    While the Giant-Impact Hypothesis is the most widely accepted theory, some details are still debated. For example, the exact size and composition of the impactor, and the precise timing of the collision, remain areas of active research.

    Other theories about the Moon's origin, such as capture or fission, are considered less likely based on current evidence.

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