
mineral
Green aventurine
Quartzite dominated by quartz (SiO₂), commonly containing fuchsite mica or other inclusions
AI-generated identification · may be incorrectTypically medium green with fine glittery aventurescence, though this polished piece appears subtly sparkly; Mohs hardness 6.5–7, vitreous to dull luster, granular quartz mosaic, no prominent cleavage, specific gravity about 2.6–2.7.
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Physical properties
Typically medium green with fine glittery aventurescence, though this polished piece appears subtly sparkly; Mohs hardness 6.5–7, vitreous to dull luster, granular quartz mosaic, no prominent cleavage, specific gravity about 2.6–2.7.
Formation & geological history
Forms when quartz-rich sediment or rock recrystallizes into quartzite, with chromium-bearing fuchsite producing the green color; deposits are generally Precambrian to younger metamorphic terrains.
Uses & applications
Used for beads, cabochons, carvings, ornamental stone, countertops, and inexpensive decorative objects.
Geological facts
Aventurine’s characteristic shimmer comes from reflected light off tiny plate-like inclusions, called aventurescence; stronger sparkle generally increases desirability.
Field identification & locations
Commonly found in India, Brazil, Russia, Tanzania, and China. Identify it by its green color, quartz-like hardness, granular texture, and glitter; it should scratch glass but not quartz. The photograph alone cannot exclude dyed quartz or another green stone.
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