
mineral
Polished green aventurine (likely)
Aventurine quartz, SiO₂, colored by fuchsite or other inclusions
AI-generated identification · may be incorrectGreen, polished, translucent to opaque, with a subtle glittery sheen; quartz has Mohs hardness 7, trigonal crystal structure, vitreous luster, and no cleavage. The smooth oval shape obscures diagnostic surface details, so identification is tentative.
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Physical properties
Green, polished, translucent to opaque, with a subtle glittery sheen; quartz has Mohs hardness 7, trigonal crystal structure, vitreous luster, and no cleavage. The smooth oval shape obscures diagnostic surface details, so identification is tentative.
Formation & geological history
A natural quartz variety formed as silica-rich fluids crystallized in veins or cavities, with green mica inclusions; specimens commonly come from India, Brazil, and Russia. Its geological age depends on the deposit.
Uses & applications
Used for beads, carvings, cabochons, decorative objects, and inexpensive jewelry.
Geological facts
Aventurine’s characteristic shimmer, called aventurescence, comes from reflective mineral inclusions; fuchsite mica commonly creates the green color.
Field identification & locations
Look for a fine, scattered sparkle and hardness sufficient to scratch glass; distinguish it from dyed stones by checking for color concentrated in cracks. Polished palm stones of this size commonly sell for about $5–$25 USD.
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