
metamorphic
Serpentinite (likely veined variety)
Serpentinite; chiefly serpentine-group minerals (antigorite, lizardite, chrysotile), commonly with magnetite and carbonate veins
AI-generated identification · may be incorrectDark greenish-black, fine-grained, waxy to subvitreous luster with pale cream/yellow veining; hardness about 2.5–4 Mohs, typically massive with no obvious cleavage, and specific gravity roughly 2.5–2.7. The apparent veins may be carbonate, silica, or altered mineral fractures.
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Physical properties
Dark greenish-black, fine-grained, waxy to subvitreous luster with pale cream/yellow veining; hardness about 2.5–4 Mohs, typically massive with no obvious cleavage, and specific gravity roughly 2.5–2.7. The apparent veins may be carbonate, silica, or altered mineral fractures.
Formation & geological history
Forms when ultramafic mantle rocks such as peridotite undergo hydration and metamorphic alteration, commonly along tectonic plate boundaries and fault zones. Ages vary widely from Precambrian to modern oceanic settings.
Uses & applications
Used as decorative and architectural stone, carvings, lapidary material, and historically as a source of asbestos-bearing serpentinite; most hand specimens have modest value.
Geological facts
Serpentinite is California’s state rock and commonly records ancient oceanic lithosphere or mantle material exposed by tectonic uplift.
Field identification & locations
Identify by its dark green-black color, smooth/waxy feel, relatively low hardness, and pale vein network; it may scratch with a steel knife and can show a green streak or magnetic response if magnetite-rich. Common in California, the Appalachians, New Zealand, Italy, and ophiolite belts worldwide.
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