
metamorphic
Greenstone pebble, likely serpentine or altered basalt
Probably serpentinite (serpentine-group minerals, Mg₃Si₂O₅(OH)₄) or chlorite-rich greenschist
AI-generated identification · may be incorrectSmooth, water-worn oval with mottled dark olive-green color and dull to slightly waxy luster; likely Mohs 2.5–4.5, with no visible crystals or cleavage. Exact identification requires hardness, streak, density, and possibly microscopy or X-ray analysis.
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Physical properties
Smooth, water-worn oval with mottled dark olive-green color and dull to slightly waxy luster; likely Mohs 2.5–4.5, with no visible crystals or cleavage. Exact identification requires hardness, streak, density, and possibly microscopy or X-ray analysis.
Formation & geological history
Likely formed by low- to moderate-temperature hydrothermal alteration of ultramafic rock, or metamorphism of basalt; ages vary widely from Precambrian to recent geologic settings. Its rounded shape indicates transport and abrasion in a stream, beach, or glacial environment.
Uses & applications
Commonly collected as a polished or tumbled stone and sometimes carved; serpentine is used decoratively and occasionally as a low-cost ornamental stone. It has little value as an unverified pebble.
Geological facts
Serpentine can resemble jade, but it is generally softer and less dense; some varieties may contain asbestos-form minerals, so avoid cutting or generating dust until identified.
Field identification & locations
Look for a greasy or waxy feel, green-black mottling, and softness relative to quartz; a steel knife may scratch many serpentinites, while quartz will not. Common sources include California, Oregon, Italy, New Zealand, and serpentinite belts worldwide.
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