Theia (planet)

An artist's depiction of the hypothetical impact of a planet like Theia and the Earth

Theia (/ˈθə/) is a hypothesized ancient planet in the early Solar System which, according to the giant-impact hypothesis, collided with the early Earth around 4.5 billion years ago, with some of the resulting ejected debris coalescing to form the Moon.[1][2] Such a collision, with the two planets' cores and mantles fusing, could explain why Earth's core is larger than expected for a body its size. Collision simulations support the idea that the large low-shear-velocity provinces in the lower mantle may be remnants of Theia.[3][4] Theia is hypothesized to have been about the size of Mars, and may have formed in the outer Solar System and provided much of Earth's water, though this is debated.[5]

  1. ^ Wolpert, Stuart (January 12, 2017). "UCLA Study Shows the Moon is Older Than Previously Thought". scitechdaily.com. UCLA. Retrieved 23 March 2022.
  2. ^ Cite error: The named reference TheiaPothesis was invoked but never defined (see the help page).
  3. ^ Sample, Ian (November 1, 2023). "Blobs near Earth's core are remnants of collision with another planet, study says". The Guardian.
  4. ^ Cite error: The named reference NYT-20231101 was invoked but never defined (see the help page).
  5. ^ Meier, M. M. M.; Reufer, A.; Wieler, R. (2014-11-01). "On the origin and composition of Theia: Constraints from new models of the Giant Impact". Icarus. 242: 316–328. arXiv:1410.3819. Bibcode:2014Icar..242..316M. doi:10.1016/j.icarus.2014.08.003. ISSN 0019-1035.

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