Rock Identifier
Tumbled greenstone (likely serpentine or nephrite) (Serpentine-group minerals, chiefly Mg₃Si₂O₅(OH)₄; possibly nephrite, a fibrous amphibole aggregate) — metamorphic
metamorphic

Tumbled greenstone (likely serpentine or nephrite)

Serpentine-group minerals, chiefly Mg₃Si₂O₅(OH)₄; possibly nephrite, a fibrous amphibole aggregate

AI-generated identification · may be incorrect

Olive-green, rounded, and polished with a waxy to silky luster; hardness is typically 2.5–4 for serpentine and 6–6.5 for nephrite. The image is insufficient to determine cleavage, crystal structure, or specific gravity reliably.

Identified More metamorphic →
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Physical properties

Olive-green, rounded, and polished with a waxy to silky luster; hardness is typically 2.5–4 for serpentine and 6–6.5 for nephrite. The image is insufficient to determine cleavage, crystal structure, or specific gravity reliably.

Formation & geological history

Serpentine forms when ultramafic rocks undergo hydration and metamorphism, commonly in ophiolites and fault zones; nephrite forms by metamorphic alteration of magnesium-rich rocks. A precise geological age cannot be determined visually.

Uses & applications

Used as a carving and ornamental stone, beads, cabochons, and tumbled specimens; nephrite is also a valued jade material. Serpentine is used decoratively and occasionally as a low-grade building stone.

Geological facts

The smooth triangular shape and reflective surface indicate human tumbling or polishing. A scratch test, density measurement, and magnification are needed to distinguish serpentine from jade.

Field identification & locations

Common sources include California, Oregon, Canada, New Zealand, China, and Central Asia. Serpentine is generally softer and waxier; nephrite is notably tough, denser, and resists scratching by a steel file.