Rock Identifier
Tumbled green stone, likely aventurine or dyed quartz (Quartz (SiO₂), possibly fuchsite-bearing green aventurine; exact identification requires testing) — mineral
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 incorrect

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.

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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.