
metamorphic
Greenstone (likely altered basalt or metabasalt)
Chlorite–actinolite-rich metabasalt; composition commonly dominated by chlorite, actinolite, epidote, albite, and quartz
AI-generated identification · may be incorrectTypically dark green to gray-green, fine-grained, opaque, and dull to weakly silky; hardness about 5–6 Mohs, massive texture, poor cleavage, and specific gravity roughly 2.8–3.2. The specimen appears weathered and may contain rusty iron-oxide staining.
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Physical properties
Typically dark green to gray-green, fine-grained, opaque, and dull to weakly silky; hardness about 5–6 Mohs, massive texture, poor cleavage, and specific gravity roughly 2.8–3.2. The specimen appears weathered and may contain rusty iron-oxide staining.
Formation & geological history
Forms when basaltic lava or mafic volcanic rock undergoes low-grade greenschist-facies metamorphism, commonly during Precambrian to Phanerozoic tectonic alteration. Exact age cannot be determined from the photograph.
Uses & applications
Used locally as crushed aggregate, landscaping stone, building stone, and occasionally as a polished ornamental material; generally little gem value.
Geological facts
“Greenstone” is a field and commercial term rather than one precise mineral species; similar-looking material may also be serpentinite or chlorite-rich basalt.
Field identification & locations
Identify by its uniform green color, fine massive texture, lack of visible large crystals, and moderate hardness; a streak, acid, magnetism, and thin-section test would help distinguish it from serpentinite or jade. Common in metamorphic belts and altered volcanic terrains worldwide.
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