Rock Identifier
Greenstone / altered basalt (probable) (Chlorite–epidote–actinolite-rich metabasalt; exact identification requires testing) — metamorphic
metamorphic

Greenstone / altered basalt (probable)

Chlorite–epidote–actinolite-rich metabasalt; exact identification requires testing

AI-generated identification · may be incorrect

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.

Identified More metamorphic
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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.