Rock Identifier
Tumbled green stone, likely serpentine or aventurine (Serpentine-group mineral (Mg₃Si₂O₅(OH)₄) or quartz-rich aventurine; exact identification requires testing) — mineral
mineral

Tumbled green stone, likely serpentine or aventurine

Serpentine-group mineral (Mg₃Si₂O₅(OH)₄) or quartz-rich aventurine; exact identification requires testing

AI-generated identification · may be incorrect

Small rounded, polished pebble; olive-green, translucent to opaque, waxy/vitreous luster, no visible crystals or cleavage. Likely hardness Mohs 2.5–4 for serpentine or 6.5–7 for aventurine; specific gravity commonly 2.5–2.7.

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Physical properties

Small rounded, polished pebble; olive-green, translucent to opaque, waxy/vitreous luster, no visible crystals or cleavage. Likely hardness Mohs 2.5–4 for serpentine or 6.5–7 for aventurine; specific gravity commonly 2.5–2.7.

Formation & geological history

Serpentine forms when ultramafic rocks undergo hydration and metamorphism, commonly during tectonic alteration; aventurine forms in silica-rich hydrothermal or metamorphic environments. Ages vary widely by locality.

Uses & applications

Used as a lapidary stone, ornamental pebble, carving material, and inexpensive jewelry component; serpentine is also used decoratively in architecture.

Geological facts

The smooth shape indicates human tumbling rather than natural weathering. A steel knife or glass-scratch test can help distinguish softer serpentine from harder quartz-rich aventurine, but may damage the specimen.

Field identification & locations

Common sources include California, Vermont, Italy, New Zealand, India, Brazil, and Russia. Look for serpentine’s waxy feel and softness versus aventurine’s glassier luster and ability to scratch glass.