
metamorphic
Likely serpentine-rich metamorphic rock
Serpentinite; chiefly serpentine-group minerals (Mg₃Si₂O₅(OH)₄), possibly with magnetite and chlorite
AI-generated identification · may be incorrectSmall dark green-gray, fine-grained, weakly lustrous specimen with a mottled texture. Serpentine has Mohs hardness about 2.5–4, no consistent cleavage, and commonly forms compact or waxy masses; the photo alone cannot confirm exact mineralogy.
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Physical properties
Small dark green-gray, fine-grained, weakly lustrous specimen with a mottled texture. Serpentine has Mohs hardness about 2.5–4, no consistent cleavage, and commonly forms compact or waxy masses; the photo alone cannot confirm exact mineralogy.
Formation & geological history
Forms when ultramafic mantle rocks such as peridotite are hydrated and metamorphosed, commonly along oceanic crust and tectonic plate boundaries. Serpentinization ranges from ancient Precambrian events to modern seafloor alteration.
Uses & applications
Used as ornamental stone, carvings, architectural stone, and historically as a source of asbestos minerals; attractive pieces are collected, though fibrous varieties should not be cut or powdered.
Geological facts
Often shows dark green to black color, slick or waxy surfaces, and may attract a magnet if magnetite is abundant. It can be confused with greenstone, jade, or chlorite-rich rocks.
Field identification & locations
Common in California, Italy, New Zealand, Canada, and ophiolite belts worldwide; test cautiously for softness and waxy texture, but laboratory testing is needed for reliable identification and asbestos screening.
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