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16.4.7: Heliodor

  • Page ID
    4036
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    Heliodor
    Chemical composition Be3Al2(SiO3)6Beryllium aluminum silicate
    Crystal system Hexagonal
    Habit Prismatic
    Cleavage Poor, basal
    Fracture Conchoidal to uneven
    Hardness 7.5
    Optic nature Uniaxial -
    Refractive index 1.57 - 1.58
    Birefringence 0.004 - 0.009
    Dispersion Low, 0.014
    Specific gravity 2.7 - 2.9
    Lustre Vitreous
    Pleochroism Weak to moderate (shades of body color)

    Heliodor is the golden yellow or golden green variety of the mineral beryl. It is a beryllium aluminum silicate. The golden color is produced when iron replaces some of the aluminum in the crystal structure. Heliodor can contain trace amounts of uranium, making it slightly radioactive. Heliodor was discovered in Namibia in 1910 in a pegmatite that also produced aquamarine, which is also colored by iron.
    Crystals form very distinct hexagonal prisms that are some of the largest crystal examples in gemology. The largest faceted heliodor, 2,054 carats, is on display at the Smithsonian Institution in Washington D.C.
    The name heliodor is Greek, meaning "gift from the sun". This stone is not often used in jewelry because it lacks brilliance and fire. Heliodor is found in Minas Gerais and Goias in Brazil, in Ukraine in Russia, and also in Connecticut and Maine in USA.
    Heliodor is considered a talisman for those named Hugh.


    This page titled 16.4.7: Heliodor is shared under a CC BY-NC-SA 2.5 license and was authored, remixed, and/or curated by gemology via source content that was edited to the style and standards of the LibreTexts platform; a detailed edit history is available upon request.

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