
metamorphic
Tumbled green-blue stone, likely serpentine or chlorite-rich metamorphic rock
Serpentinite (mainly antigorite/lizardite; identification is image-based)
AI-generated identification · may be incorrectTypically Mohs 2.5–4, dark green to blue-green, mottled, waxy to greasy luster, and fine-grained with no visible crystal faces; specific gravity about 2.5–2.6. The rounded surface indicates tumbling or natural abrasion.
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Physical properties
Typically Mohs 2.5–4, dark green to blue-green, mottled, waxy to greasy luster, and fine-grained with no visible crystal faces; specific gravity about 2.5–2.6. The rounded surface indicates tumbling or natural abrasion.
Formation & geological history
Forms when ultramafic mantle rocks such as peridotite undergo hydration and metamorphism, commonly in ancient or active tectonic zones; ages vary widely. Its blue-green appearance may also reflect chlorite, magnetite, or other accessory minerals.
Uses & applications
Used as an ornamental and carving stone, tumbled-stone material, and historically in architecture; attractive pieces may be sold as decorative specimens. Avoid dust from cutting because some serpentinite can contain asbestos-form minerals.
Geological facts
Serpentinite often shows black magnetite specks and a slippery, waxy feel. It may be weakly magnetic and can be confused with nephrite, chlorite schist, or dyed material.
Field identification & locations
Common in ophiolite belts and mountain regions, including California, the Alps, New Zealand, and the Appalachians. Field confirmation requires hardness, streak, magnetism, and ideally microscopy or spectroscopy.
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