
metamorphic
Likely green-gray serpentine-bearing rock
Serpentinite, dominated by serpentine-group minerals (antigorite/lizardite; Mg₃Si₂O₅(OH)₄), possibly with chlorite or talc
AI-generated identification · may be incorrectDark green-gray, mottled, fine-grained and dull to waxy; typically Mohs 2.5–4, with poor cleavage and uneven fracture. The photograph is insufficient for confident identification; texture may also fit chlorite- or talc-rich metamorphic rock.
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Physical properties
Dark green-gray, mottled, fine-grained and dull to waxy; typically Mohs 2.5–4, with poor cleavage and uneven fracture. The photograph is insufficient for confident identification; texture may also fit chlorite- or talc-rich metamorphic rock.
Formation & geological history
Forms when ultramafic mantle rocks such as peridotite hydrate during low-temperature metamorphism and hydrothermal alteration, commonly in ophiolites and subduction zones. Formation ages vary widely from Precambrian to modern tectonic settings.
Uses & applications
Used as decorative stone, carvings, countertops, and sometimes aggregate; attractive varieties are collected, though fibrous asbestos-bearing material should not be cut or powdered.
Geological facts
Serpentinite often has a smooth, greasy or waxy feel and may contain magnetite, giving it a dark color or weak magnetic response.
Field identification & locations
Check for a waxy feel, low hardness, green veining, and reaction to a steel knife; talc-rich pieces scratch very easily. Common localities include California, Italy, New Zealand, Canada, and Japan.
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