Rock Identifier
Polished green aventurine (likely serpentine or quartzite) (Aventurine quartz, SiO₂; appearance may also resemble serpentinite, mainly Mg₃Si₂O₅(OH)₄) — metamorphic
metamorphic

Polished green aventurine (likely serpentine or quartzite)

Aventurine quartz, SiO₂; appearance may also resemble serpentinite, mainly Mg₃Si₂O₅(OH)₄

AI-generated identification · may be incorrect

Light green, finely streaked, opaque-to-translucent slab with waxy to vitreous polish; quartz aventurine has Mohs hardness 6.5–7, while serpentine is softer at 2.5–5.5. The image lacks diagnostic crystal or cleavage features.

Identified More metamorphic
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Physical properties

Light green, finely streaked, opaque-to-translucent slab with waxy to vitreous polish; quartz aventurine has Mohs hardness 6.5–7, while serpentine is softer at 2.5–5.5. The image lacks diagnostic crystal or cleavage features.

Formation & geological history

Green aventurine forms when quartz crystallizes with fuchsite mica; serpentinite forms by hydrothermal alteration of ultramafic rocks, commonly during oceanic crust or mountain-building processes. Precise age and identification require testing.

Uses & applications

Used for countertops, tiles, decorative slabs, carvings, and cabochons; market value depends strongly on color, pattern, thickness, and whether it is genuine aventurine quartz.

Geological facts

The broad pale-green, flowing texture is especially characteristic of decorative serpentine or green quartzite slabs, often sold commercially under broad trade names such as “green marble.”

Field identification & locations

Check hardness, streak, density, acid reaction, and a fresh edge: quartz scratches glass, whereas serpentine usually does not. Common sources include Brazil, India, China, Italy, and the United States.