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  2. Theia (planet) - Wikipedia

    en.wikipedia.org/wiki/Theia_(planet)

    According to the giant impact hypothesis, Theia orbited the Sun, nearly along the orbit of the proto-Earth, by staying close to one or the other of the Sun-Earth system's two more stable Lagrangian points (i.e., either L 4 or L 5). [8] Theia was eventually perturbed away from that relationship, most likely by the gravitational influence of ...

  3. Giant-impact hypothesis - Wikipedia

    en.wikipedia.org/wiki/Giant-impact_hypothesis

    [2] [14] According to modern theories of planet formation, Theia was part of a population of Mars-sized bodies that existed in the Solar System 4.5 billion years ago. One of the attractive features of the giant-impact hypothesis is that the formation of the Moon and Earth align; during the course of its formation, Earth is thought to have ...

  4. Relics of huge primordial collision reside in Earth's deep ...

    www.aol.com/news/relics-huge-primordial...

    The researchers ran computer simulations examining the impact event, geophysical properties of the material that likely made up Theia and the evolution of Earth's mantle - the broadest of the ...

  5. Scientists say they’ve finally found remnants of Theia, an ...

    www.aol.com/collision-formed-moon-created-alien...

    Theia, an ancient planet, collided with Earth to form the moon, scientists believe. A new study suggests Theia could have also formed mysterious blobs called large low-velocity provinces, or LLVPs.

  6. 2% of Earth's Mass May Be Debris From the Massive ... - AOL

    www.aol.com/2-earths-mass-may-debris-161400172.html

    4.5 billion years ago, Earth experienced a cataclysmic rendezvous with a planet named Theia. Evidence of the impact is still buried deep within the Earth. 2% of Earth's Mass May Be Debris From the ...

  7. Chaotian (geology) - Wikipedia

    en.wikipedia.org/wiki/Chaotian_(geology)

    A revised proposal in 2012 [2] suggested the Chaotian as the first era of the Hadean representing the time between the formation of the Solar System c. 4.567 Ga [3] and the oldest preserved crustal material on Earth, a detrital zircon c. 4.404 Ga [4] from the Jack Hills of the Narryer terrane in Western Australia.

  8. Co-orbital configuration - Wikipedia

    en.wikipedia.org/wiki/Co-orbital_configuration

    These include 54509 YORP, (85770) 1998 UP 1, 2002 AA 29, (419624) 2010 SO 16, 2009 BD, and 2015 SO 2 which exist in resonant orbits similar to Cruithne's. 2010 TK 7 and (614689) 2020 XL 5 are the only two identified Earth trojans. Hungaria asteroids were found to be one of the possible sources for co-orbital objects of the Earth with a lifetime ...

  9. Titius–Bode law - Wikipedia

    en.wikipedia.org/wiki/Titius–Bode_law

    Let the distance from the Sun to Saturn be taken as 100, then Mercury is separated by 4 such parts from the Sun. Venus is 4+3=7. The Earth 4+6=10. Mars 4+12=16. Now comes a gap in this so orderly progression. After Mars there follows a space of 4+24=28 parts, in which no planet has yet been seen.