
mineral
Polished blue-green stone, likely chrysocolla or chrysocolla-bearing chalcedony
Chrysocolla: hydrated copper phyllosilicate, approximately (Cu,Al)₂H₂Si₂O₅(OH)₄·nH₂O; exact identification requires testing
AI-generated identification · may be incorrectBlue-green, opaque, waxy to dull luster, commonly amorphous or microcrystalline; Mohs hardness 2–4 for chrysocolla, higher if mixed with chalcedony. The smooth oval shape indicates tumbling or cabochon polishing.
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Physical properties
Blue-green, opaque, waxy to dull luster, commonly amorphous or microcrystalline; Mohs hardness 2–4 for chrysocolla, higher if mixed with chalcedony. The smooth oval shape indicates tumbling or cabochon polishing.
Formation & geological history
Forms as a secondary copper-mineral deposit during weathering and oxidation, often coating or replacing host rock. Commonly associated with malachite, azurite, quartz, and limonite in relatively young near-surface ore zones.
Uses & applications
Used for cabochons, beads, carvings, and collector specimens; harder chrysocolla-chalcedony varieties are preferred for jewelry. Soft material should be protected from scratches, chemicals, and prolonged soaking.
Geological facts
Its vivid color comes from copper; color intensity and hardness vary greatly with quartz content. It may be confused with turquoise, variscite, or dyed agate.
Field identification & locations
Common sources include Arizona, Nevada, Chile, Peru, Mexico, Australia, and the Democratic Republic of the Congo. Field clues are blue-green color and copper-mineral association; hardness and streak testing help distinguish it from turquoise.
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