Rock Identifier
Tumbled green stone, likely aventurine or dyed agate (Tentatively quartz-rich green aventurine (SiO₂) or chrysoprase (microcrystalline chalcedony, SiO₂); identification is uncertain from the image) — mineral
mineral

Tumbled green stone, likely aventurine or dyed agate

Tentatively quartz-rich green aventurine (SiO₂) or chrysoprase (microcrystalline chalcedony, SiO₂); identification is uncertain from the image

AI-generated identification · may be incorrect

Opaque to translucent vivid green, polished/tumbled, with a waxy to vitreous luster and apparent fractures or inclusions. Quartz varieties have Mohs hardness about 6.5–7 and specific gravity near 2.6; possible dyeing cannot be excluded.

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Physical properties

Opaque to translucent vivid green, polished/tumbled, with a waxy to vitreous luster and apparent fractures or inclusions. Quartz varieties have Mohs hardness about 6.5–7 and specific gravity near 2.6; possible dyeing cannot be excluded.

Formation & geological history

Aventurine forms when quartz crystallizes with fuchsite or other green inclusions; chrysoprase forms as nickel-bearing chalcedony in weathered ultramafic environments. These materials are geologically young to ancient depending on the host deposit.

Uses & applications

Used for beads, cabochons, ornaments, and inexpensive decorative stones; polished pieces have modest lapidary value.

Geological facts

The intense, fairly uniform color and rounded polish may indicate dyed quartz, serpentine, or another treated stone rather than natural high-grade chrysoprase.

Field identification & locations

Check for glittery fuchsite reflections (aventurine), waxy translucence (chrysoprase), scratches against glass, and color concentration in cracks; definitive identification requires testing or laboratory analysis. Common sources include India, Brazil, Russia, Australia, and Madagascar.