
mineral
Tumbled green stone, likely aventurine or dyed quartz
Quartz (SiO₂), possibly fuchsite-bearing green aventurine; exact identification requires testing
AI-generated identification · may be incorrectSmall polished/tumbled specimen with dark green color and vitreous-to-waxy luster. Quartz hardness is Mohs 7, with no cleavage, conchoidal fracture, and specific gravity about 2.65; the image is insufficient to confirm composition or treatments.
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Physical properties
Small polished/tumbled specimen with dark green color and vitreous-to-waxy luster. Quartz hardness is Mohs 7, with no cleavage, conchoidal fracture, and specific gravity about 2.65; the image is insufficient to confirm composition or treatments.
Formation & geological history
Green aventurine forms when quartz crystallizes with fuchsite or other green inclusions in metamorphic or hydrothermal environments; quartz-bearing rocks commonly formed over millions to billions of years. Similar stones may be dyed chalcedony or serpentine.
Uses & applications
Used as a decorative tumbled stone, ornamental material, and inexpensive jewelry bead; collector value is generally low unless unusually vivid, translucent, or naturally chatoyant.
Geological facts
Natural aventurine commonly shows fine glitter (aventurescence) from mica inclusions, while dyed stones often have unnaturally uniform color or color concentrated in fractures.
Field identification & locations
Check for sparkle, translucency, hardness, and color stability; quartz should scratch glass, though this test can damage the specimen. Common sources include India, Brazil, Russia, and Zimbabwe.
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