
metamorphic
Tumbled serpentine with magnetite/chromite veining
Serpentinite; chiefly serpentine-group minerals, Mg₃Si₂O₅(OH)₄, with opaque magnetite or chromite
AI-generated identification · may be incorrectTypically Mohs 2.5–4, waxy to greasy luster, pale green-yellow to brown with black veins or patches, and fine-grained massive structure; no visible cleavage. The wet, polished appearance and black mineral inclusions fit serpentine, though image-only identification is provisional.
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Physical properties
Typically Mohs 2.5–4, waxy to greasy luster, pale green-yellow to brown with black veins or patches, and fine-grained massive structure; no visible cleavage. The wet, polished appearance and black mineral inclusions fit serpentine, though image-only identification is provisional.
Formation & geological history
Forms when ultramafic mantle rocks such as peridotite are hydrated during hydrothermal alteration, commonly in ophiolites and subduction zones. Ages vary widely, from ancient Precambrian bodies to modern alteration zones.
Uses & applications
Used as ornamental stone, beads, carvings, and occasionally architectural stone; softer pieces are popular tumbled specimens. Avoid prolonged exposure to dust from cutting, particularly if asbestos-form serpentine minerals are present.
Geological facts
The black material may be magnetite or chromite; magnetite can be weakly magnetic. Serpentinite is often mottled, slick-looking, and associated with chromite deposits.
Field identification & locations
Look for low hardness, waxy luster, green-yellow coloration, and black veining; a steel nail may scratch it, unlike jade. Common in California, Italy, New Zealand, Canada, and ophiolite belts worldwide.
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