
metamorphic
Polished greenstone (likely serpentine or altered basalt)
Serpentinite, mainly serpentine-group minerals (Mg₃Si₂O₅(OH)₄); exact identification requires testing
AI-generated identification · may be incorrectDark green to gray-green, matte to waxy luster, fine-grained and rounded with pinkish veins or patches. Mohs hardness about 2.5–5.5; cleavage generally absent, density commonly 2.5–2.7 g/cm³.
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Physical properties
Dark green to gray-green, matte to waxy luster, fine-grained and rounded with pinkish veins or patches. Mohs hardness about 2.5–5.5; cleavage generally absent, density commonly 2.5–2.7 g/cm³.
Formation & geological history
Likely formed by hydrothermal alteration of magnesium-rich ultramafic rock, commonly during ancient oceanic or tectonic processes; geological age cannot be determined from the image.
Uses & applications
Used as ornamental stone, carvings, cabochons, and occasionally architectural facing; attractive green varieties are collected but usually modestly priced.
Geological facts
Serpentinite can resemble jade, but it is generally softer and less dense. Pink veins may consist of carbonate minerals or iron-rich alteration products.
Field identification & locations
Look for a greasy or waxy surface, green coloration, low hardness, and pale or pink veining; a steel nail may scratch many specimens. Common in ophiolite belts and metamorphic terrains worldwide.
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