
metamorphic
Rounded greenish stone, possibly serpentinite or greenstone
Likely serpentinite (hydrated ultramafic rock; chiefly serpentine-group minerals), but the photograph is insufficient for confident species identification
AI-generated identification · may be incorrectFine-grained, olive-green to gray-green, dull to subtly waxy luster, rounded/tumbled surface; serpentine has Mohs hardness about 2.5–4 and no obvious cleavage. The specimen appears roughly 1–2 cm across; density is commonly about 2.5–2.6 g/cm³.
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Physical properties
Fine-grained, olive-green to gray-green, dull to subtly waxy luster, rounded/tumbled surface; serpentine has Mohs hardness about 2.5–4 and no obvious cleavage. The specimen appears roughly 1–2 cm across; density is commonly about 2.5–2.6 g/cm³.
Formation & geological history
Serpentinite forms when mantle-derived peridotite is hydrothermally altered by water, commonly along convergent-plate boundaries and fault zones; ages range from Precambrian to modern tectonic settings. Its color and texture can also resemble chlorite-rich greenstone or altered basalt.
Uses & applications
Used as decorative stone, carvings, and occasionally jewelry; larger serpentinite masses are used for architectural facing and ornamental objects. This small piece has mainly educational or modest collecting value.
Geological facts
Serpentinite commonly contains magnetite and may be weakly magnetic; some varieties contain chrysotile asbestos, so avoid cutting, drilling, or generating dust until tested.
Field identification & locations
Look for an olive-green color, smooth waxy feel, mottled veins, and relatively low hardness; a steel nail may scratch it. Common occurrences include California, Vermont, New Zealand, Italy, and ophiolite belts worldwide.
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