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  • Ferromagnesian Silicates: Properties, Examples & Uses
    Ferromagnesian silicates are a group of minerals that are rich in iron (Fe) and magnesium (Mg) and contain silicate (SiO4) tetrahedra. They are typically dark-colored and have a relatively high density. Here are some examples:

    Common Ferromagnesian Silicates:

    * Olivine: A very common mineral found in the Earth's mantle. It is typically green to olive-green in color and has a glassy luster.

    * Pyroxene: A group of minerals with a variety of compositions and colors. Common pyroxenes include augite (black), hypersthene (brown), and diopside (green).

    * Amphibole: Another group of minerals with a variety of compositions and colors. Common amphiboles include hornblende (black), actinolite (green), and tremolite (white).

    * Biotite: A black mica mineral that is often found in igneous and metamorphic rocks.

    * Hornblende: A black amphibole mineral commonly found in igneous and metamorphic rocks.

    Less Common Ferromagnesian Silicates:

    * Enstatite: A colorless to brown pyroxene mineral.

    * Anthophyllite: A white to brown amphibole mineral.

    * Gedrite: A brown to black amphibole mineral.

    * Cummingtonite: A brown to black amphibole mineral.

    Note: This is not an exhaustive list, as there are many other ferromagnesian silicates. However, these are some of the most common and well-known examples.

    Ferromagnesian silicates are important components of many rocks, including igneous, metamorphic, and sedimentary rocks. They are also important in the Earth's mantle and crust.

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