
metamorphic
Polished green tumbled stone, likely serpentine
Serpentinite (rock composed chiefly of serpentine-group minerals, approximately Mg₃Si₂O₅(OH)₄)
AI-generated identification · may be incorrectSmall, rounded, opaque olive-green specimen with a smooth polish and subdued waxy luster. Serpentine minerals have Mohs hardness about 2.5–5.5; the image alone does not confirm the identification or specific gravity.
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Physical properties
Small, rounded, opaque olive-green specimen with a smooth polish and subdued waxy luster. Serpentine minerals have Mohs hardness about 2.5–5.5; the image alone does not confirm the identification or specific gravity.
Formation & geological history
Serpentinite forms when water alters magnesium-rich rocks, commonly at oceanic crust and mantle settings; its age varies with the host rocks and alteration. The specimen has been shaped and polished, obscuring diagnostic natural texture.
Uses & applications
Tumbled serpentinite is used for decoration, lapidary crafts, and inexpensive jewelry; larger serpentinite deposits are also quarried as ornamental stone.
Geological facts
Serpentine is a mineral group rather than one single mineral, and serpentinite can contain several serpentine minerals.
Field identification & locations
The olive color and waxy polish are consistent with serpentinite, but other green stones can look similar; hardness, streak, and mineral tests would help distinguish them. Serpentinite occurs in many mountain belts and former oceanic crust zones worldwide.
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