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  2. As Earth began to take shape about 4.5 billion years ago, iron and nickel quickly separated from other rocks and minerals to form the core of the new planet. The molten material that surrounded the core was the early mantle. Over millions of years, the mantle cooled. Water trapped inside minerals erupted with lava, a process called “ outgassing.”
    www.nationalgeographic.org/encyclopedia/mantle/
    www.nationalgeographic.org/encyclopedia/mantle/
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  4. WEBApr 30, 2024 · The mantle is the mostly solid bulk of Earth’s interior. The mantle lies between Earth’s dense, superheated core and its thin outer layer, the crust. The mantle is about 2,900 kilometers (1,802 miles) …

     
  5. WEBBy combining available geological and geochemical observations with geodynamical considerations, a tentative hypothesis is presented for the …

    • Author: Jun Korenaga
    • Publish Year: 2018
  6. WEBSep 25, 2019 · Our compilation reveals that—before about 200 million years ago (Ma)—the mantle source of all kimberlite bodies globally appears to …

    • Author: Jon Woodhead, Janet Hergt, Andrea Giuliani, Andrea Giuliani, Andrea Giuliani, Roland Maas, David Phi...
    • Publish Year: 2019
  7. WEBEarth's mantle is a layer of silicate rock between the crust and the outer core. It has a mass of 4.01 × 10 24 kg (8.84 × 10 24 lb) and makes up 67% of the mass of Earth. [1] It has a thickness of 2,900 kilometers (1,800 …

  8. New study supports stable mantle chemistry dating back to …

  9. Mantle (geology) - Wikipedia

  10. Evolution of the mantle (Chapter 6) - The Earth

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  19. Earth Mantle - an overview | ScienceDirect Topics

  20. The Chemical Evolution of the Earth's Mantle - Scientific American

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  22. Earth’s thermal evolution, mantle convection, and Hadean onset …

  23. History of Earth - Wikipedia

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  28. Mass extinction 66 million years ago triggered rapid evolution of …

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