
metamorphic
Green tumbled stone, possibly serpentine
Likely serpentine-group rock, chiefly serpentine minerals (approx. Mg₃Si₂O₅(OH)₄); identification is uncertain from the photograph.
AI-generated identification · may be incorrectSmall, rounded, translucent-to-opaque pale olive-green pebble with a waxy or dull luster and mottled appearance. Serpentine has Mohs hardness about 2.5–5 and a monoclinic crystal structure; hardness and cleavage cannot be determined from the image.
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Physical properties
Small, rounded, translucent-to-opaque pale olive-green pebble with a waxy or dull luster and mottled appearance. Serpentine has Mohs hardness about 2.5–5 and a monoclinic crystal structure; hardness and cleavage cannot be determined from the image.
Formation & geological history
Serpentine forms when magnesium-rich ultramafic rocks are altered by water, commonly during metamorphism; such rocks range widely in age and occur in mountain belts and oceanic crust.
Uses & applications
Serpentine is used as ornamental stone, carvings, and some jewelry; softer pieces are mainly decorative or collectible.
Geological facts
Green color alone is not diagnostic: jade, quartz, glass, and other stones can look similar. A reliable identification may require hardness, specific-gravity, or laboratory testing.
Field identification & locations
The smooth, rounded shape suggests tumbling or water wear. Serpentine is common in ultramafic-rock belts worldwide; avoid scratch or chemical tests on a potentially valuable piece.
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