LABRADORITE

VOLGA BLUE CLASSIC

Labradorite forms deep within the Earth’s crust through the cooling of magma. This process involves the crystallization of minerals rich in calcium and sodium, creating plagioclase feldspar. The stunning iridescence, known as labradorescence, is due to thin layers within the crystal that refract and scatter light. Over millions of years, geological processes bring these beautiful stones to the surface, where they can be mined and admired for their unique play of colors

characteristics

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Structure

Volga Blue has a massive texture, coarse-grained structures, irrigating crystals in blue and yellow-green colors

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Non-Hygroscopic

Labradorite does not absorb moisture, making it ideal for various environments

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Durability

Labradorite is resistant to atmospheric and domestic temperature changes

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Surface Integrity

The stone remains free of stains and minor mechanical damages