Igneous Rock Crystallization Quiz
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Questions and Answers

Which mineral typically crystallizes first from cooling magma?

  • Biotite
  • Amphibole
  • Olivine (correct)
  • Pyroxene
  • What is the term for the sequence in which minerals crystallize from magma?

  • Geothermal gradient
  • Felsic series
  • Igneous classification
  • Bowen reaction series (correct)
  • What mineral reacts with olivine as the temperature of the magma decreases?

  • Quartz
  • Pyroxene (correct)
  • Amphibole
  • Biotite
  • Which variety of plagioclase feldspar crystallizes first at high temperatures?

    <p>Anorthite</p> Signup and view all the answers

    As the temperature of the magma decreases, which mineral will form if sodium is still available?

    <p>Sodium-rich plagioclase</p> Signup and view all the answers

    Study Notes

    Igneous Rock Crystallization

    • Minerals in igneous rocks crystallize at varying temperatures, meaning a cooling magma can contain crystals while still being mostly liquid.

    • The Bowen reaction series describes the order in which minerals crystallize from cooling magma.

    • Olivine, a common silicate mineral, is the first to crystallize, typically between 1200° and 1300°C.

    • As the magma cools and silica remains, olivine reacts with silica to form pyroxene.

    • The discontinuous branch of the Bowen reaction series follows this pattern: olivine → pyroxene → amphibole → biotite.

    • Plagioclase feldspar begins crystallization around the same temperature as pyroxene.

    • Initial plagioclase crystals are calcium-rich (anorthite). As the temperature drops and sodium remains in the magma, the plagioclase becomes more sodium-rich.

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    Description

    Test your understanding of the crystallization process of minerals in igneous rocks. This quiz covers the Bowen reaction series, the temperatures at which different minerals crystallize, and the transformations that occur as magma cools. Challenge yourself with questions related to olivine, pyroxene, and plagioclase feldspar.

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