
metamorphic
Rounded yellow-green stone, likely serpentine or weathered greenstone
Serpentine-group minerals, commonly antigorite or lizardite; exact identification requires testing
AI-generated identification · may be incorrectOpaque olive-yellow green, dull to waxy luster, smoothly rounded and probably water-worn; likely Mohs hardness 2.5–4, with no visible crystals or cleavage. Specific gravity is commonly about 2.5–2.6.
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Physical properties
Opaque olive-yellow green, dull to waxy luster, smoothly rounded and probably water-worn; likely Mohs hardness 2.5–4, with no visible crystals or cleavage. Specific gravity is commonly about 2.5–2.6.
Formation & geological history
Serpentine forms when ultramafic rocks such as peridotite are hydrated during metamorphism, commonly in ophiolites and fault zones; its age depends on the host terrain. The rounded shape indicates later stream or beach transport.
Uses & applications
Usually collected as a curiosity or lapidary stone; suitable pieces may be polished for cabochons or carvings, but this small specimen has little industrial value.
Geological facts
The image alone cannot distinguish serpentine from epidote-rich greenstone, altered basalt, or another weathered rock. Some serpentine rocks may contain fibrous chrysotile, so avoid cutting, grinding, or creating dust until tested.
Field identification & locations
Look for a greasy or waxy feel, green-to-yellow color, low hardness, and possible white veining; a steel nail may scratch it. Common settings include California, Oregon, Italy, New Zealand, and ophiolite belts worldwide.
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