
metamorphic
Tumbled greenstone/serpentinite pebble
Serpentinite, chiefly antigorite/lizardite Mg₃Si₂O₅(OH)₄; identification is visual and uncertain
AI-generated identification · may be incorrectDark olive-green, rounded and polished, with a dull to waxy luster and fine-grained texture. Typical hardness is 2.5–4 Mohs, no visible cleavage, and specific gravity about 2.5–2.6.
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Physical properties
Dark olive-green, rounded and polished, with a dull to waxy luster and fine-grained texture. Typical hardness is 2.5–4 Mohs, no visible cleavage, and specific gravity about 2.5–2.6.
Formation & geological history
Forms when ultramafic mantle rocks such as peridotite undergo low-temperature hydration and metamorphism, commonly in ancient oceanic crust and subduction zones. Serpentinite occurrences range from Precambrian to modern geological settings.
Uses & applications
Used as ornamental stone, carvings, beads, countertops, and landscaping material; attractive specimens are collected as polished pebbles. It is generally less durable than jade and should not be confused with true jadeite or nephrite.
Geological facts
The image shows a strongly rounded, likely tumbled specimen; exact identification cannot be confirmed without hardness, streak, density, or mineralogical testing. Some serpentinite contains chrysotile asbestos, so avoid cutting, drilling, or generating dust.
Field identification & locations
Common in ophiolites and alpine/subduction belts, including California, Italy, New Zealand, Canada, and Japan. A waxy feel, green mottling, low hardness, and possible white veining support serpentinite; jade is harder (about 6–7 Mohs).
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