
metamorphic
Greenstone / altered basalt (probable)
Chlorite–epidote–actinolite-rich metabasalt; exact identification requires testing
AI-generated identification · may be incorrectDark green-gray, mottled, fine-grained, and dull to slightly waxy; likely hardness about 5–6, with no obvious cleavage and a dense, compact texture. The pale green matrix may contain chlorite, epidote, actinolite, or serpentine.
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Physical properties
Dark green-gray, mottled, fine-grained, and dull to slightly waxy; likely hardness about 5–6, with no obvious cleavage and a dense, compact texture. The pale green matrix may contain chlorite, epidote, actinolite, or serpentine.
Formation & geological history
Typically formed when basaltic lava undergoes low-grade metamorphism or hydrothermal alteration, commonly in ancient oceanic crust and volcanic belts. Geological age cannot be determined from the photograph.
Uses & applications
Used locally as building or landscaping stone and occasionally as a carving or lapidary material; ordinary pieces have little jewelry value.
Geological facts
“Greenstone” is a broad field term rather than one precise mineral or rock. Similar-looking specimens include serpentinite, greenschist, altered granite, and jade-like rocks.
Field identification & locations
Look for a dense green color, mottling, fine grain, and possible white veins; a streak, hardness, magnetism, specific gravity, and thin-section test would improve identification. Common in metamorphic belts and altered volcanic terrains.
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