
metamorphic
Greenstone, likely altered basalt (possibly serpentinite)
Metabasalt/greenschist; commonly chlorite–actinolite–epidote ± serpentine
AI-generated identification · may be incorrectDark green-gray, fine-grained, dull to faintly silky luster, massive texture, and no obvious cleavage; approximate hardness 5–6 if metabasalt, or 3–5 if serpentinite. Identification is limited by the photograph; the pale streaks may be alteration minerals.
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Physical properties
Dark green-gray, fine-grained, dull to faintly silky luster, massive texture, and no obvious cleavage; approximate hardness 5–6 if metabasalt, or 3–5 if serpentinite. Identification is limited by the photograph; the pale streaks may be alteration minerals.
Formation & geological history
Likely basalt altered by low- to moderate-grade metamorphism during seafloor hydrothermal alteration or regional metamorphism, commonly in ancient oceanic crust and accretionary belts. Exact geological age cannot be determined visually.
Uses & applications
Used locally as landscaping stone, carving material, or aggregate; attractive pieces may be sold as decorative greenstone, though this specimen appears ordinary rather than gem quality.
Geological facts
“Greenstone” is a broad field term rather than one precise mineral or rock. Chlorite and epidote commonly produce green color in metamorphosed basalt, while serpentine gives a waxier appearance and lower hardness.
Field identification & locations
Look for a heavy, compact green rock with a fine texture; a steel nail test, streak test, and acid reaction can help distinguish it from softer serpentinite or carbonate rock. Common settings include ophiolites, greenstone belts, and metamorphic mountain belts.
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