
metamorphic
Tumbled dark-green serpentine
Serpentinite; chiefly serpentine-group minerals, commonly antigorite, lizardite, or chrysotile (Mg₃Si₂O₅(OH)₄)
AI-generated identification · may be incorrectTypically dark green to black, waxy-to-greasy luster, massive and fine-grained, with Mohs hardness about 2.5–4 and specific gravity around 2.5–2.6. The specimen shows polishing, fractures, and mottled green-black veining.
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Physical properties
Typically dark green to black, waxy-to-greasy luster, massive and fine-grained, with Mohs hardness about 2.5–4 and specific gravity around 2.5–2.6. The specimen shows polishing, fractures, and mottled green-black veining.
Formation & geological history
Forms when ultramafic mantle rocks such as peridotite are hydrated during hydrothermal alteration, commonly along plate boundaries and ancient oceanic crust. Individual serpentinite bodies range from Precambrian to modern geological ages.
Uses & applications
Used as a decorative and carving stone, ornamental aggregate, and historically as a source of asbestos-bearing material; attractive pieces are sold as lapidary specimens and jewelry.
Geological facts
Serpentinite is often mistaken for jade, but it is generally softer and less tough. Chrysotile-bearing varieties can release hazardous fibers when cut or abraded.
Field identification & locations
Identify by its low hardness, waxy feel, dark green color, and inability to scratch glass reliably; common localities include California, Italy, New Zealand, Canada, and the Himalaya. Avoid dry cutting or drilling unless asbestos content is excluded.
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