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  2. Feb 18, 2020 · This is a table that shows the elemental chemical composition of the Earth's crust. Keep in mind, these numbers are estimates. They will vary depending on the way they were calculated and the source. 98.4% of the Earth's crust consists of oxygen, silicon, aluminum, iron, calcium

  3. Oct 30, 2023 · Oxygen is the most abundant element in the Earth’s crust, at 461,000 parts per million. This means it makes up roughly 46% of the Earth’s crust. Within the universe at large, Oxygen ranks number three in abundance. Oxygen makes up 21% of the Earth’s atmosphere and 90% of the mass of water.

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  4. May 23, 2018 · This table and periodic table shows the relative abundance of elements in the Earth’s crust. Each element is represented by its atomic number, symbol, name, and abundance in milligrams per kilogram of Earth’s crust.

    Number
    Element
    Abundance (mg/l)
    8
    4.61 x 10 5
    14
    Silicon
    2.82 x 10 5
    13
    Aluminum
    8.23 x 10 4
    26
    5.63 x 10 4
  5. Dec 14, 2021 · Many elements make up the crust, with some, like oxygen and iron, being more abundant than others. Oxygen, silicon, iron and aluminum are the most abundant elements in the Earth's crust, accounting for 88.1% of its mass.

  6. The abundance of elements in Earth's crust is shown in tabulated form with the estimated crustal abundance for each chemical element shown as mg/kg, or parts per million (ppm) by mass (10,000 ppm = 1%). Reservoirs. The Earth's crust is one "reservoir" for measurements of abundance.

    Z
    Element
    Symbol
    Goldschmidt Classification
    8
    O
    Lithophile
    14
    Si
    Lithophile
    13
    Al
    Lithophile
    26
    Fe
    Siderophile
  7. The most common chemical elements in the crust are oxygen (46.6%), silicon (27.7), aluminum (8.1), iron (5.0), calcium (3.6), potassium (2.8), sodium (2.6), and magnesium (2.1). These figures vary among different studies because we really have no way to know for sure.

  8. Jan 21, 2023 · The crust. The outermost part of the earth, known also as the lithosphere, is broken up into plates that are supported by the underlying mantle, and are moved by the convective cells within the mantle at a rate of a few centimetres per year.

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