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16.10: Feldspar

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    Chemical composition Potassium, sodium and calcium-aluminum silicates

    I. K-feldspar (KALSi308)
    II . Plagioclase feldspar (isomorphous)

    Crystal system Monoclinic - triclinic
    Habit Prismatic, often twinned
    Cleavage Good to perfect
    Fracture Conchoidal
    Hardness 6
    Optic nature Biaxial ±
    Refractive index 1.52 - 1.53 (K-feldspar)

    1.528 - 1.588 (plagioclase)

    Birefringence 0.006 - 0.007 (K-feldspar)

    0.008 - 0.011 (plagioclase)

    Specific gravity 2.55 - 2,58 (K-feldspar)

    2.60 - 2.80 (plagioclase)

    Lustre Vitreous

    Feldspar is a group of minerals that are very important in rock formation, accounting for over half of Earth's crust! There are a number of varieties that are used in jewelry. The most important are andesine, sunstone, amazonite, moonstone, and labradorite, the latter two known for their phenomenal adularescence and iridescence. Amazonite was used by the ancient Egyptians for carving images of deities, the stone considered a catalyst between the living and the gods. Moonstone was thought to drive away sleeplessness.

    Feldspars are divided into two types:

    • K-feldspars (potassium feldspars)
    • Plagioclase feldspars (an isomorphous series between albite and anorthite)

    Feldspar comp triangle.jpg

    Figure \(\PageIndex{1}\)


    K-feldspars grow in monoclinic crystals (except for microcline) and have a chemical composition of KAlSi3O8.


    • Orthoclase
    • Orthoclase moonstone
    • Microcline (amazonite)
    • Sanidine

    Plagioclase feldspar

    Plagioclase feldspars grow in triclinic crystals. Its varieties belong to an isomorphous series between albite (NaAlSi3O8) and anorthite (CaAl2Si2O8).


    • Albite (100-90% albite, 0-10% anorthite)
    • Oligoclase (90-70% albite, 10-30% anorthite)
    • Andesine (70-50% albite, 30-50% anorthite)
    • Labradorite (50-30% albite, 50-70% anorthite)
    • Bytownite (30-10% albite, 70-90% anorthite)
    • Anorthite (10-0% albite, 90-100% anorthite)

    Figure \(\PageIndex{2}\): Timeline image indicating the percentages of the albite-anorthite series

    "Confetti" sunstone

    "Confetti" sunstone is oligoclase feldspar in composition. The background color can be colorless, yellow, orange, or light green. The colorful flashes are caused by flecks or platelets of hematite. Faceted stones of good size with no fractures and plenty of hematite inclusions are always a treat to see. Tanzania is the only source we know of for this interesting gem.


    Figure \(\PageIndex{3}\): Confetti sunstone (by Scott Davies)


    Figure \(\PageIndex{4}\): Confetti sunstone (by Scott Davies)


    Figure \(\PageIndex{4}\): Confetti sunstone (by Scott Davies)

    Short Films

    Remarkable, outstanding, exceptional—Bill Larson had an extraordinary orthoclase specimen on view at the 2009 Westward Look Show in Tucson. Dave Wilber brings us on a personalized tour of some highlights in Bill Larson's collection, including a large (we mean really big) transparent yellow orthoclase crystal from Madagascar.

    Spectacular Amazonite Crystals
    Joe Dorris from Pinnacle 5 Minerals, Glacier Peak Mining, talks to Wilber about the amazonite and smoky quartz specimens from Colorado.
    Amazonite and Smoky quartz is a classic association. The specimens pictured here are astounding examples.

    Links for Further Feldspar Information

    Causes of Color in Amazonite

    This page titled 16.10: Feldspar 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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