### Origin of the Moon
Three scientific models have been proposed to explain the origin of the Moon:
* Fission Model: The Moon was once part of the Earth but was thrown off early in the solar system's history due to the Earth's rapid rotation. Since it split directly from the young Earth's mantle, the Moon's chemical composition (such as oxygen isotope ratios) should be identical to Earth's mantle, and its orbit should lie along Earth's equatorial plane.
* Capture Model: The Moon formed independently elsewhere in the solar system, with its own unique composition, and was later captured by Earth's gravity during a close pass. This model suggests that the Moon's chemical composition should be distinct from Earth's.
* Giant Impact Model: A Mars-sized protoplanet collided with the young Earth. The impact blasted debris from both the protoplanet and Earth's outer mantle into orbit, which then accreted to form the Moon. Because the Moon formed from mantle debris, it should have a very low iron content compared to Earth, which retained its massive iron core.
Match each new scientific finding and the model evaluated to its correct relationship (whether the finding supports, contradicts, or has no effect on that model).
- Finding: Lunar rock samples show oxygen isotope ratios that are completely identical to Earth's mantle. Model evaluated: Capture Model.Contradicts the evaluated model
- Finding: Seismic data indicates the Moon's iron core constitutes less than 3% of its mass, while Earth's is 30%. Model evaluated: Giant Impact Model.Supports the evaluated model
- Finding: The lunar surface is covered in a layer of regolith (rocky dust) created by meteorite impacts. Model evaluated: Fission Model.Has no effect on the evaluated model