
metamorphic
Dark green metamorphic stone, likely serpentinite
Serpentinite; primarily serpentine-group minerals, Mg₃Si₂O₅(OH)₄, possibly with magnetite, chlorite, or talc
AI-generated identification · may be incorrectFine- to medium-grained, massive, dark green to gray-green, with dull to waxy luster and no obvious crystals or cleavage; Mohs hardness typically 2.5–4, specific gravity about 2.5–2.6. The photograph is consistent with serpentinite, though a definitive identification requires testing.
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Physical properties
Fine- to medium-grained, massive, dark green to gray-green, with dull to waxy luster and no obvious crystals or cleavage; Mohs hardness typically 2.5–4, specific gravity about 2.5–2.6. The photograph is consistent with serpentinite, though a definitive identification requires testing.
Formation & geological history
Forms when ultramafic mantle rocks such as peridotite hydrate during metamorphism, commonly along faults and seafloor subduction zones; specimens may range from Precambrian to modern tectonic settings.
Uses & applications
Used as decorative facing stone, carvings, countertops, and occasionally jewelry; softer material is mainly valued for ornamental and lapidary work rather than structural construction.
Geological facts
Serpentinite commonly contains mesh-like serpentine textures and may weather to a smooth, dark-green surface. Some specimens contain asbestos-form serpentine minerals, so avoid cutting or generating dust unless composition is confirmed.
Field identification & locations
Field clues include green color, low hardness, waxy feel, and association with ophiolites or ultramafic rocks; a steel knife may scratch it, while dilute acid typically produces little reaction. Common localities include California, Italy, New Zealand, and Canada.
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