
metamorphic
Polished green-gray stone, possibly serpentine
Likely serpentine-group rock, composed mainly of serpentine minerals; identification is uncertain from the photo
AI-generated identification · may be incorrectOpaque, mottled green-gray with a polished, waxy-to-greasy luster. Serpentine has Mohs hardness about 2.5–5.5 and commonly forms massive material without visible crystals; hardness and composition cannot be confirmed visually.
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Physical properties
Opaque, mottled green-gray with a polished, waxy-to-greasy luster. Serpentine has Mohs hardness about 2.5–5.5 and commonly forms massive material without visible crystals; hardness and composition cannot be confirmed visually.
Formation & geological history
Serpentine forms when magnesium-rich ultramafic rocks are altered by water, commonly during metamorphism at or near tectonic plate boundaries. Such rocks range widely in age.
Uses & applications
Polished serpentine is used for carvings, beads, ornaments, and decorative stone; softer material is generally unsuitable for demanding construction uses.
Geological facts
The smooth oval shape indicates the specimen has been shaped and polished; appearance alone cannot reliably distinguish serpentine from other green stones such as jade or aventurine.
Field identification & locations
Look for mottled green color, relatively low hardness, and a waxy feel; a scratch test or mineralogical testing would help confirm identity. Serpentinite occurs in many mountain belts worldwide.
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