Rock Identifier
Polished green aventurine (likely serpentine or nephrite imitation) (Aventurine quartz, SiO₂, if genuine; visually also consistent with serpentine, Mg₃Si₂O₅(OH)₄) — mineral
mineral

Polished green aventurine (likely serpentine or nephrite imitation)

Aventurine quartz, SiO₂, if genuine; visually also consistent with serpentine, Mg₃Si₂O₅(OH)₄

AI-generated identification · may be incorrect

Pale mint-green, opaque to slightly translucent, vitreous-to-waxy luster, smoothly faceted and polished; aventurine quartz has Mohs hardness 6.5–7, while serpentine is softer at 2.5–5.5. No visible sparkle or diagnostic crystal structure is apparent.

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Physical properties

Pale mint-green, opaque to slightly translucent, vitreous-to-waxy luster, smoothly faceted and polished; aventurine quartz has Mohs hardness 6.5–7, while serpentine is softer at 2.5–5.5. No visible sparkle or diagnostic crystal structure is apparent.

Formation & geological history

Green aventurine forms when chromium-bearing mica or fuchsite occurs in quartz during metamorphic or hydrothermal processes; serpentine forms by hydration of ultramafic rocks. Geological ages vary widely by deposit.

Uses & applications

Used for carvings, beads, cabochons, ornamental objects, and inexpensive jewelry; this appears to be a polished pendant or carving.

Geological facts

The image alone cannot reliably distinguish aventurine from similarly colored serpentine, jade, dyed quartz, or glass. Strong glitter suggests aventurine; waxy appearance and lower hardness suggest serpentine.

Field identification & locations

Common sources include India, Brazil, Russia, China, and Zimbabwe. Test cautiously with hardness, streak, magnification, and specific gravity; avoid scratching valuable material.