
metamorphic
Greenstone (likely serpentinite or altered basalt)
Serpentinite, predominantly serpentine-group minerals (Mg₃Si₂O₅(OH)₄); possibly chlorite- or actinolite-rich greenschist
AI-generated identification · may be incorrectDark olive-green, fine-grained, dull to slightly waxy luster, massive texture, and no obvious crystal faces or cleavage. Typical hardness is Mohs 2.5–4; exact identification requires hardness, streak, magnetism, and specific-gravity tests.
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Physical properties
Dark olive-green, fine-grained, dull to slightly waxy luster, massive texture, and no obvious crystal faces or cleavage. Typical hardness is Mohs 2.5–4; exact identification requires hardness, streak, magnetism, and specific-gravity tests.
Formation & geological history
Most likely formed by low- to moderate-temperature metamorphic alteration of ultramafic rock or basalt during hydration and tectonic activity. Such rocks range from Precambrian to modern plate-boundary settings.
Uses & applications
Commonly used as decorative stone, carvings, beads, and occasionally architectural facing; specimen value is usually modest unless it has attractive veining or unusual texture.
Geological facts
“Greenstone” is a broad field term rather than one mineral species; visually similar rocks include serpentinite, greenschist, chlorite schist, and altered basalt.
Field identification & locations
Look for a green color, fine granular texture, and waxy feel; serpentinite may show pale veins and can produce a white streak. Common localities include California, Italy, New Zealand, Canada, and oceanic suture zones.
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