
metamorphic
Green aventurine quartz (likely rough quartzite)
Quartz, SiO₂, with green mica/fuchsite or chlorite inclusions
AI-generated identification · may be incorrectTranslucent pale green-gray, vitreous to slightly waxy luster, massive granular texture, and no obvious cleavage; quartz hardness is Mohs 7, with specific gravity about 2.65. The rounded shape may reflect natural water wear or tumbling/polishing.
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Physical properties
Translucent pale green-gray, vitreous to slightly waxy luster, massive granular texture, and no obvious cleavage; quartz hardness is Mohs 7, with specific gravity about 2.65. The rounded shape may reflect natural water wear or tumbling/polishing.
Formation & geological history
Most likely quartz-rich metamorphic rock (quartzite) or massive quartz formed when silica-rich fluids recrystallized older rocks; green color comes from mica or chlorite inclusions. Exact geological age and locality cannot be determined from the image.
Uses & applications
Used as ornamental stone, carvings, beads, cabochons, tumbled stones, and decorative aggregate; less commonly used as quartzite building stone.
Geological facts
Aventurine’s characteristic sparkle, called aventurescence, is caused by reflective mineral inclusions; this specimen appears only weakly sparkly and could alternatively be green-stained or inclusion-rich quartz.
Field identification & locations
Look for glassy translucence, hardness sufficient to scratch ordinary glass, and green reflective flakes; it should not fizz in dilute acid. Common sources include India, Brazil, Russia, and China.
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