
metamorphic
Polished dark green stone, likely serpentinite or chlorite schist
Serpentinite (Mg-rich serpentine minerals, commonly antigorite/lizardite) or chlorite-rich schist
AI-generated identification · may be incorrectDark green to black, fine-grained, waxy-to-submetallic luster with pale reflective flecks; typically Mohs 2.5–4 for serpentinite (chlorite schist about 2–3), massive or weakly foliated, with no obvious cleavage visible. The rounded shape indicates tumbling or polishing.
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Physical properties
Dark green to black, fine-grained, waxy-to-submetallic luster with pale reflective flecks; typically Mohs 2.5–4 for serpentinite (chlorite schist about 2–3), massive or weakly foliated, with no obvious cleavage visible. The rounded shape indicates tumbling or polishing.
Formation & geological history
Forms when ultramafic mantle rocks such as peridotite undergo hydration and metamorphism, commonly in ancient oceanic crust and tectonic suture zones; individual pieces may range from Precambrian to much younger. Exact identification and age require testing or microscopy.
Uses & applications
Used as ornamental stone, carvings, counters, and collectible tumbled material; some serpentinite is marketed as “new jade,” though it is not jadeite or nephrite. Common pieces generally have modest commercial value.
Geological facts
Serpentinite often shows a greasy or waxy surface and may contain magnetite, producing dark specks or slight magnetism. Chlorite-rich rocks can look similar but are usually more distinctly flaky or schistose.
Field identification & locations
Check for a waxy feel, green-black color, soft scratchability with a steel nail, and possible magnetism; avoid acid-based identification. Common localities include California, Italy, New Zealand, Canada, and tectonic mountain belts worldwide.
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