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Igneous Rocks Classification Flashcards
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Igneous Rocks Classification Flashcards

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Questions and Answers

What two characteristics are used to classify igneous rocks?

Texture and composition

Igneous rocks with large crystals exhibit a ______ texture.

coarse-grained

What kind of texture do igneous rocks exhibit when they cool rapidly?

  • Fine-grained Texture (correct)
  • Glassy Texture
  • Coarse-grained Texture
  • Porphyritic Texture
  • What is an example of a rock with a glassy texture?

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

    Rocks that have a ______ composition are typically darker and denser than granitic rocks.

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

    What is the main mineral composition of granitic rocks?

    <p>Quartz and feldspar</p> Signup and view all the answers

    Match the following compositional groups with their characteristics:

    <p>Granitic = Contains about 70 percent silica Basaltic = Rich in magnesium and iron Andesitic = Composition between granitic and basaltic Ultramafic = Composed almost entirely of dark silicate minerals</p> Signup and view all the answers

    Porphyritic texture results from minerals crystallizing at the same rate.

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

    What is the common volcanic rock associated with andesitic composition?

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

    Study Notes

    Classification of Igneous Rocks

    • Igneous rocks are classified by texture and composition.
    • Texture refers to appearance regarding crystal size, shape, and arrangement.
    • Composition classification is based on the proportion of light (silicate) and dark minerals.

    Coarse-Grained Texture

    • Slow cooling of magma leads to the formation of large crystals.
    • This process allows ions to move long distances within the magma.
    • Rocks with this texture display a coarse-grained appearance due to substantial crystal sizes.

    Fine-Grained Texture

    • Rapid cooling of magma or lava results in small, interconnected mineral grains.
    • Ions in quickly cooled magma lose motion, promoting fast mineral formation.
    • The competition for available ions creates a large number of tiny crystals.

    Glassy Texture

    • Rapid cooling of lava on the Earth's surface prevents crystallization.
    • Resulting rocks consist of randomly distributed ions instead of crystalline structures.
    • Obsidian and pumice are prime examples of rocks with a glassy texture.

    Porphyritic Texture

    • Crystals in magma crystallize at different rates, leading to varied sizes.
    • Larger crystals, known as phenocrysts, can form before smaller crystals.
    • This texture features large and small minerals due to different cooling rates.

    Granitic Composition

    • Granitic rocks are predominantly composed of light-colored silicate minerals like quartz and feldspar.
    • They contain about 70% silica and are prevalent in continental crust.
    • Rhyolite is an example of an extrusive granitic rock.

    Basaltic Composition

    • Basaltic rocks are rich in dark silicate minerals and plagioclase feldspar.
    • These rocks contain high levels of magnesium and iron, making them darker and denser.
    • Basalt is the most common basaltic rock, while gabbro is its intrusive equivalent.

    Other Compositional Groups

    • Andesitic composition represents a blend between granitic and basaltic rocks, named after andesite.
    • Peridotite, a significant igneous rock, consists mainly of olivine and pyroxene.
    • Classified as ultramafic, peridotite is primarily made of dark silicate minerals.

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    Test your knowledge on the classification of igneous rocks with these flashcards. Explore key terms such as texture and composition, and understand how these characteristics help identify various igneous rock types.

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