
mineral
Tumbled green stones, likely green aventurine or serpentine
Quartzite with fuchsite inclusions (green aventurine), or serpentine-group minerals; exact identification requires testing
AI-generated identification · may be incorrectOpaque green-gray, rounded and polished, with waxy to subtly sparkling luster; likely Mohs 3–7 depending on composition, with no obvious cleavage and granular or fibrous texture
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Physical properties
Opaque green-gray, rounded and polished, with waxy to subtly sparkling luster; likely Mohs 3–7 depending on composition, with no obvious cleavage and granular or fibrous texture
Formation & geological history
Green aventurine forms when quartz recrystallizes with mica inclusions, commonly during metamorphism; serpentine forms by hydrothermal alteration of ultramafic rocks. Specimens may be geologically ancient, but age depends on locality
Uses & applications
Used as inexpensive lapidary material, carvings, cabochons, tumbled stones, décor, and occasionally construction aggregate; typically modest collector value
Geological facts
Aventurine’s green color commonly comes from fuchsite mica, while serpentine’s color comes from iron and nickel-bearing minerals; a glassy sparkle favors aventurine
Field identification & locations
Common sources include India, Brazil, Russia, China, and the United States. Aventurine scratches glass weakly to readily (about Mohs 6–7); serpentine is much softer and may be scratched by a steel knife