
metamorphic
Greenstone (likely serpentinite or altered basalt)
Serpentinite, chiefly serpentine-group minerals; possibly chlorite- or actinolite-bearing greenschist
AI-generated identification · may be incorrectDark olive-green, fine-grained, opaque to slightly translucent, with a dull to waxy luster and indistinct cleavage; estimated Mohs hardness 3–5. The irregular pale veining and mottled texture are typical of serpentinization or low-grade metamorphism.
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Physical properties
Dark olive-green, fine-grained, opaque to slightly translucent, with a dull to waxy luster and indistinct cleavage; estimated Mohs hardness 3–5. The irregular pale veining and mottled texture are typical of serpentinization or low-grade metamorphism.
Formation & geological history
Most likely formed by hydrothermal alteration of ultramafic rock, or metamorphism of basalt, during ancient oceanic crust and subduction-related processes; the specimen’s exact age cannot be determined from the image.
Uses & applications
Used as decorative stone, carving material, landscaping aggregate, and historically as a source rock for asbestos-bearing minerals; attractive polished pieces may be sold as ornamental stone.
Geological facts
“Greenstone” is a broad field term rather than a single mineral or rock. Serpentinite commonly contains magnetite and may show weak magnetic response; avoid cutting or sanding unknown material because some varieties contain fibrous asbestos minerals.
Field identification & locations
Common in ophiolites and metamorphic belts worldwide, including California, New England, Italy, New Zealand, and the Alps. A waxy feel, low hardness, green color, and pale veining support serpentinite, but laboratory testing is needed for a definitive identification.
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