
metamorphic
Tumbled greenstone or serpentine pebble
Serpentinite, chiefly serpentine-group minerals (Mg₃Si₂O₅(OH)₄); possibly nephrite jade if notably tough and dense
AI-generated identification · may be incorrectSmooth, rounded, pale yellow-green surface with dull to waxy luster and faint veining; likely Mohs 3–6, with no visible crystals or cleavage. Exact identification requires hardness, density, and translucency tests.
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Physical properties
Smooth, rounded, pale yellow-green surface with dull to waxy luster and faint veining; likely Mohs 3–6, with no visible crystals or cleavage. Exact identification requires hardness, density, and translucency tests.
Formation & geological history
Serpentinite forms when ultramafic mantle rocks undergo hydration during metamorphism, commonly in ophiolites and subduction zones; the specimen is likely naturally water-worn or tumbled. Its precise geological age cannot be determined from the image.
Uses & applications
Commonly used as decorative stone, carvings, beads, and landscaping material; higher-quality nephrite jade is used in jewelry and sculpture.
Geological facts
Serpentine and jade can look similar, but jade is substantially tougher and generally denser. Avoid acid or destructive tests; a steel scratch test and specific-gravity measurement are more useful.
Field identification & locations
Common in California, New Zealand, Italy, Canada, Russia, and ultramafic terrains worldwide; identify by green color, waxy feel, veining, and relatively low hardness. The photograph alone cannot distinguish serpentine from low-grade jade or another greenstone.
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