
metamorphic
Tumbled green serpentine (likely nephrite jade imitation/alternative)
Serpentine-group minerals, chiefly antigorite and lizardite; composition approximately Mg₃Si₂O₅(OH)₄
AI-generated identification · may be incorrectDark olive-green, semi-translucent edges, waxy to greasy luster, massive rather than visibly crystalline, with conchoidal-to-uneven fractures; Mohs hardness about 2.5–4, specific gravity roughly 2.5–2.6. The rectangular form and rounded edges indicate cutting and polishing.
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Physical properties
Dark olive-green, semi-translucent edges, waxy to greasy luster, massive rather than visibly crystalline, with conchoidal-to-uneven fractures; Mohs hardness about 2.5–4, specific gravity roughly 2.5–2.6. The rectangular form and rounded edges indicate cutting and polishing.
Formation & geological history
Formed when ultramafic mantle rocks undergo low-temperature hydration and metamorphism, commonly in subduction-zone mélanges; most examples are Paleozoic to younger, though age cannot be determined from the image.
Uses & applications
Used for carvings, beads, cabochons, decorative stone, and sometimes marketed as “new jade.” It is softer and generally less valuable than true jadeite or nephrite.
Geological facts
The specimen may also be low-grade nephrite or another green stone; image-only identification is provisional. A refractive index, hardness, specific gravity, and microscopic examination would separate these possibilities.
Field identification & locations
Common sources include California, New Zealand, China, Afghanistan, and Italy. Serpentine typically has a softer feel and scratches more easily than nephrite; avoid acids and ultrasonic cleaning.
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