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    Which feature of the chemical differentiation of Earth today reflects the influence of the iron catastrophe?
    Question

    Which feature of the chemical differentiation of Earth today reflects the influence of the iron catastrophe?

    A.

    There is more iron in the core than in the crust.

    B.

    The lower lithosphere stores most of Earth's iron.

    C.

    Much of Earth's iron has escaped as a result of extraterrestrial impacts.

    D.

    Iron is rare in Earth.

    Correct option is A

    Explanation:
    The iron catastrophe refers to a pivotal event in Earth's early history (around 4.5 billion years ago) when the planet was still molten. During this time:
    · Heavy elements like iron and nickel sank toward the center due to gravity.
    · Lighter silicate minerals rose to form the mantle and crust.
    As a result, Earth's core became highly enriched in iron, while the crust contains relatively less.
    This process is a prime example of chemical differentiation, where Earth's internal structure (core, mantle, crust) was formed based on the density and composition of elements.
    Information Booster:
    · The core is composed mostly of iron (Fe) and nickel (Ni).
    · The mantle is rich in silicate minerals containing magnesium and iron.
    · The crust contains a mix of silicates, but much less metallic iron.
    Additional Information:
    · (b) is incorrect: The core, not the lithosphere, holds most of the iron.
    · (c) is incorrect: Earth's iron did not escape — it sank to the core.
    · (d) is incorrect: Iron is not rare in Earth; it's one of the most abundant elements in the planet.

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