Rock Identifier
Greenstone, likely altered basalt (possibly serpentinite) (Metabasalt/greenschist; commonly chlorite–actinolite–epidote ± serpentine) — metamorphic
metamorphic

Greenstone, likely altered basalt (possibly serpentinite)

Metabasalt/greenschist; commonly chlorite–actinolite–epidote ± serpentine

AI-generated identification · may be incorrect

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.

Identified More metamorphic
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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.