
metamorphic
Tumbled greenstone/serpentine pebble
Serpentinite, chiefly serpentine-group minerals (Mg₃Si₂O₅(OH)₄), possibly with chlorite or talc
AI-generated identification · may be incorrectPale green, rounded, opaque, and dull to waxy with a fine-grained massive texture; serpentine has Mohs hardness about 2.5–4 and no visible cleavage. The photograph is insufficient to confirm composition, and similar-looking greenstones include nephrite and altered volcanic rock.
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Physical properties
Pale green, rounded, opaque, and dull to waxy with a fine-grained massive texture; serpentine has Mohs hardness about 2.5–4 and no visible cleavage. The photograph is insufficient to confirm composition, and similar-looking greenstones include nephrite and altered volcanic rock.
Formation & geological history
Typically forms when ultramafic mantle rocks are hydrated and metamorphosed, commonly in oceanic lithosphere and subduction-zone mélanges; ages range from Precambrian to modern tectonic settings.
Uses & applications
Used as decorative stone, carvings, beads, and minor architectural material; high-quality tougher varieties may be sold as greenstone, while ordinary pebbles have little commercial value.
Geological facts
Serpentinite often shows mottled green coloration and a slippery or waxy feel; some varieties contain magnetite and may be weakly magnetic.
Field identification & locations
Field clues include low hardness, pale green streak or powder, waxy luster, and reaction to neither dilute acid nor a steel knife strongly; hardness and density testing can distinguish it from jade. Common in ophiolites and tectonic fault zones.
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