Rock Identifier
Polished green cabochon, likely aventurine or serpentine (Quartz aventurine (SiO₂) or serpentine-group mineral; visual identification is uncertain) — mineral
mineral

Polished green cabochon, likely aventurine or serpentine

Quartz aventurine (SiO₂) or serpentine-group mineral; visual identification is uncertain

AI-generated identification · may be incorrect

Opaque to translucent dark green, vitreous-to-waxy luster, smoothly polished cabochon with no visible crystal faces. Aventurine has Mohs hardness 6.5–7; serpentine is softer, about 2.5–5.5, and typically shows a waxier surface.

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Physical properties

Opaque to translucent dark green, vitreous-to-waxy luster, smoothly polished cabochon with no visible crystal faces. Aventurine has Mohs hardness 6.5–7; serpentine is softer, about 2.5–5.5, and typically shows a waxier surface.

Formation & geological history

Green aventurine forms when chromium- or fuchsite-bearing quartz crystallizes in metamorphic or hydrothermal veins; serpentine forms by hydration of ultramafic rocks. Both are generally Precambrian to younger, depending on locality.

Uses & applications

Used for beads, cabochons, carvings, ornaments, and inexpensive jewelry; serpentine is also used decoratively as a soapstone-like material.

Geological facts

The even dark-green color and lack of obvious glitter make serpentine or dyed chalcedony possible; a scratch, specific-gravity, or refractive-index test is needed for confident identification.

Field identification & locations

Common sources include India, Brazil, Russia, China, and the United States. Check for tiny mica sparkles, hardness, and translucency; glassy conchoidal fracture favors chalcedony, while waxy softness favors serpentine.