
mineral
Green aventurine (likely)
Quartz, SiO₂, with green fuchsite inclusions
AI-generated identification · may be incorrectOpaque to translucent green, vitreous-to-dull luster; quartz has Mohs hardness 7 and a trigonal crystal structure, with no cleavage and conchoidal fracture. The pictured rough, rounded piece is not diagnostic, so identification is tentative.
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Physical properties
Opaque to translucent green, vitreous-to-dull luster; quartz has Mohs hardness 7 and a trigonal crystal structure, with no cleavage and conchoidal fracture. The pictured rough, rounded piece is not diagnostic, so identification is tentative.
Formation & geological history
Typically forms as quartz-bearing veins or metamorphic rocks; green color comes from tiny mica inclusions. Quartz deposits span many geological ages.
Uses & applications
Used for beads, carvings, decorative objects, and inexpensive jewelry.
Geological facts
Aventurine’s subtle glitter, called aventurescence, comes from reflective mineral inclusions; it may be hard to see in rough pieces.
Field identification & locations
Often found in India, Brazil, Russia, and elsewhere. Look for a granular, sparkly appearance and test hardness only on an inconspicuous spot; color alone cannot distinguish it from other green minerals.
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