Minerals & Rocks


  • Feldspar

    Feldspar

    Feldspar is a family of silicate minerals belonging to the tectosilicates subclass, with two primary members – alkali feldspars and plagioclase feldspars. These minerals exhibit

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  • Zeolite

    Zeolite

    Zeolites are a family of hydrated aluminosilicate minerals, belonging to the tectosilicates subclass. These unique minerals are characterized by their crystalline structures, which contain interconnected,

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  • Labradorite

    Labradorite

    Labradorite is a fascinating mineral belonging to the plagioclase feldspar group within the tectosilicates class. This captivating mineral is renowned for its remarkable optical phenomenon

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  • Plagioclase

    Plagioclase

    Plagioclase is a series of tectosilicate minerals within the feldspar family, which are some of the most abundant minerals on Earth. Characterized by its triclinic

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  • Sodalite

    Sodalite

    Sodalite is a feldspathoid mineral, belonging to the tectosilicate subclass, known for its captivating blue color and distinctive white veining. The mineral exhibits a cubic

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  • Mica

    Mica

    Mica is a group of sheet silicate minerals that belong to the phyllosilicate class. These minerals are characterized by their perfect basal cleavage, which allows

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  • Talc

    Talc

    Talc is a hydrous magnesium silicate mineral, belonging to the phyllosilicate class of minerals. Notable for being the softest mineral on the Mohs hardness scale,

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  • Chlorite

    Chlorite

    Chlorite is a group of phyllosilicate minerals characterized by their sheet-like structures and green color. These minerals belong to the chlorite group within the larger

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  • Serpentine

    Serpentine

    Serpentine is a group of hydrous magnesium silicate minerals that belong to the phyllosilicate class. These minerals exhibit a wide range of physical characteristics, including

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  • Biotite

    Biotite

    Biotite is a phyllosilicate mineral belonging to the mica group and is a common component of various igneous, metamorphic, and sedimentary rocks. It is characterized

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