Rock Identifier
Polished dark stone, likely nephrite jade or serpentine (Tentatively nephrite (fibrous amphibole aggregate, Ca₂(Mg,Fe)₅Si₈O₂₂(OH)₂); possibly serpentine) — mineral
mineral

Polished dark stone, likely nephrite jade or serpentine

Tentatively nephrite (fibrous amphibole aggregate, Ca₂(Mg,Fe)₅Si₈O₂₂(OH)₂); possibly serpentine

AI-generated identification · may be incorrect

Small rounded, highly polished dark green-black specimen with waxy to vitreous luster and mottled green highlights. Nephrite has Mohs hardness 6–6.5, no visible cleavage, tough interlocking fibers, and specific gravity about 2.9–3.1; the photograph cannot confirm identity.

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Physical properties

Small rounded, highly polished dark green-black specimen with waxy to vitreous luster and mottled green highlights. Nephrite has Mohs hardness 6–6.5, no visible cleavage, tough interlocking fibers, and specific gravity about 2.9–3.1; the photograph cannot confirm identity.

Formation & geological history

Nephrite forms through metamorphic alteration and metasomatism of ultramafic or calcium-rich rocks, commonly in serpentinite zones; deposits range from Paleozoic to younger. Serpentine forms by hydration of mantle-derived peridotite.

Uses & applications

Used for cabochons, beads, carvings, and ornamental objects; nephrite is valued for exceptional toughness, while ordinary serpentine is mainly decorative or architectural.

Geological facts

The dark color may result from iron-rich amphibole or magnetite inclusions. A polished surface obscures texture, so visual identification alone is provisional.

Field identification & locations

Check translucency, uniformity, heft, and a fibrous or interlocking texture under magnification; hardness and density testing, plus Raman or thin-section analysis, are more reliable. Common sources include British Columbia, Wyoming, New Zealand, China, and Russia.