epidote definition

  • noun:
    • A lustrous yellowish, green, or black colored mineral, Ca2(Al, Fe)3(SiO4)3OH, frequently found in metamorphic rock.
    • A lustrous yellowish, green, or black mineral, Ca2(Al, Fe)3(SiO4)3OH, generally within metamorphic stone.
    • any one of a course of mixed calcium metal aluminum sorosilicates present in metamorphic stones
    • some of a class of blended calcium iron aluminium sorosilicates present in metamorphic rocks
    • A mineral, frequently of a yellowish green (pistachio) color, happening granular, huge, columnar, as well as in monoclinic crystals. Its a silicate of alumina, lime, and oxide of iron, or manganese.
    • A mineral, frequently of a yellowish green (pistachio) shade, occurring granular, massive, columnar, plus monoclinic crystals. It's a silicate of alumina, lime, and oxide of iron, or manganese.
    • A common mineral, occurring in prismatic crystals belonging to the monoclinic system, in addition huge, generally speaking of a pistachio-green color and of a vitreous luster.
    • a standard mineral, occurring in prismatic crystals of the monoclinic system, also massive, typically of a pistachio-green color as well as a vitreous luster.
    • A lustrous yellow, green, or black mineral, Ca2(Al, Fe)3(SiO4)3OH, frequently present in metamorphic rock.
    • A lustrous yellow, green, or black mineral, Ca2(Al, Fe)3(SiO4)3OH, generally found in metamorphic rock.
    • some of a class of blended calcium iron aluminium sorosilicates present in metamorphic rocks
    • any one of a class of mixed calcium iron aluminium sorosilicates present in metamorphic rocks
    • A mineral, commonly of a yellowish green (pistachio) color, occurring granular, massive, columnar, and in monoclinic crystals. It is a silicate of alumina, lime, and oxide of iron, or manganese.
    • A mineral, frequently of a yellowish green (pistachio) shade, happening granular, massive, columnar, and in monoclinic crystals. It is a silicate of alumina, lime, and oxide of iron, or manganese.
    • a typical mineral, happening in prismatic crystals belonging to the monoclinic system, in addition huge, generally of a pistachio-green shade as well as a vitreous luster.
    • A common mineral, happening in prismatic crystals of the monoclinic system, also massive, generally speaking of a pistachio-green shade as well as a vitreous luster.

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