
metamorphic
Greenstone (likely chlorite- or epidote-rich metamorphic rock)
Greenstone; commonly metamorphosed basalt or dolerite, with chlorite, epidote, and actinolite
AI-generated identification · may be incorrectDark olive-green, fine-grained, with a granular to slightly sparkly surface; likely Mohs 5–6, though exact hardness and mineral content cannot be confirmed from the image. Greenstone has no single crystal structure or characteristic cleavage because it is a mixture of minerals.
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Physical properties
Dark olive-green, fine-grained, with a granular to slightly sparkly surface; likely Mohs 5–6, though exact hardness and mineral content cannot be confirmed from the image. Greenstone has no single crystal structure or characteristic cleavage because it is a mixture of minerals.
Formation & geological history
Forms when basaltic rocks are altered by low-grade metamorphism and hydrothermal fluids. Such rocks occur in ancient volcanic belts of many geological ages.
Uses & applications
Used as decorative stone, landscaping material, and occasionally for carvings or jewelry; ordinary hand specimens have little commercial value.
Geological facts
The name “greenstone” describes color and alteration, not one precise mineral or rock composition.
Field identification & locations
Look for a dense, fine-grained green rock, often with tiny pale or dark mineral flecks; it may occur in metamorphic belts and altered volcanic terrains. Image-based identification is tentative; a hardness test or thin-section analysis would help distinguish it from other green rocks.
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