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Labradorite - Wikipedia, the free encyclopedia
Labradorite ((Ca, Na)(Al, Si) 4 O 8), a feldspar mineral, is an intermediate to calcic member of the plagioclase series. It is usually defined as having "%An" between 50 and 70.
Plagioclase - Wikipedia, the free encyclopedia
Labradorite frequently shows an iridescent display of colors due to light refracting within the lamellae of the crystal. It is named after Labrador, where it is a constituent of the ...
Labradorite Beads - Fire Mountain Gems and Beads
Faceted surfaces take these colorful gems to a higher, glistening design level. Since these are cut from freeform slabs, please note that sizes will vary.
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A huge collection of high quality blue flash labradorite beads necklaces and handcrafted labradorite silver necklaces at very cheap prices. Check out our labradorite ...
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Labradorite is a feldspar which displays a schiller called labradorescence in lustrous ... Labradorite Iridescence. History of Sunstone. Calibrated ...
Gemstones - Labradorite | Artbeads.com
Free Shipping in the U.S. The subtle flashes of iridescence found in labradorite make it a favorite among beaders. Mix with Swarovski crystal for a truly radiant piece.
How to Labradorite & Healing | eHow.com
How to article - labradorite & healing. Labradorite is a very unique looking stone. It is generally sold in its polished form. It is grayish in color or can be black,
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We sell high quality natural blue fire labradorite stone rings in handcrafted silver at very affordable prices. Our prices are cheap as we source the stones ourselves and get them ...
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Supplies of Andesine Labradorite are quite recent, with the vivid red being the ... Labradorite Iridescence. Collecting Gemstones. Calibrated Gemstone Chart ...
labradorite
Buy Labradorite direct from Norcross-Madagascar Labradorite quarry. Labradorite spheres, Labradorite carvings, Labradorite polished specimens, Labradorite rough, spectralite ...
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Labradorite ((Ca,Na)(Al,Si)4O8), a feldspar mineral, is an intermediate to calcic member of the plagioclase series. It is usually defined as having "%An" (anorthite) between 50 and 70. The specific gravity ranges from 2.71 to 2.74. The streak is white, like most silicates. The refractive index ranges from 1.555 to 1.575. Twinning is common. As with all plagioclase members the crystal system is triclinic and three directions of cleavage are present two of which form nearly right angle prisms. It occurs as clear, white to gray, blocky to lath shaped grains in common mafic igneous rocks such as basalt and gabbro, as well as in anorthosites.

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