Rock Identifier
Tumbled green stone, possibly serpentine or nephrite jade (Tentative: serpentine-group mineral (Mg₃Si₂O₅(OH)₄) or nephrite, a fibrous amphibole aggregate) — mineral
mineral

Tumbled green stone, possibly serpentine or nephrite jade

Tentative: serpentine-group mineral (Mg₃Si₂O₅(OH)₄) or nephrite, a fibrous amphibole aggregate

AI-generated identification · may be incorrect

Small rounded green specimen with a dull to waxy luster and mottled pale coloration. Serpentine is Mohs 2.5–4; nephrite is tougher and harder, about 6–6.5; crystal structure is generally concealed by fine-grained aggregates.

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Physical properties

Small rounded green specimen with a dull to waxy luster and mottled pale coloration. Serpentine is Mohs 2.5–4; nephrite is tougher and harder, about 6–6.5; crystal structure is generally concealed by fine-grained aggregates.

Formation & geological history

Serpentine forms when ultramafic rocks undergo hydration and alteration; nephrite forms through metamorphism and metasomatism in serpentinite-related rocks. Both commonly formed in ancient ophiolites and metamorphic belts.

Uses & applications

Used as decorative tumbled stone, carvings, and occasionally jewelry; confirmed jade can be valuable, while serpentine is mainly ornamental.

Geological facts

Color alone cannot reliably distinguish jade from serpentine, chrysoprase, or other green stones. Nephrite commonly shows interlocking fibrous texture under magnification and resists scratching better than serpentine.

Field identification & locations

Common sources include China, New Zealand, Canada, Russia, and the western United States. Test cautiously: a steel point may scratch serpentine but usually not quality nephrite; laboratory density, refractive index, and microscopy are more reliable.