Rock Identifier
Tumbled blue-green stone, likely chrysocolla or dyed chalcedony (Probable chrysocolla (hydrated copper aluminosilicate; variable composition), though appearance could also represent dyed chalcedony) — mineral
mineral

Tumbled blue-green stone, likely chrysocolla or dyed chalcedony

Probable chrysocolla (hydrated copper aluminosilicate; variable composition), though appearance could also represent dyed chalcedony

AI-generated identification · may be incorrect

Polished/tumbled, opaque to translucent blue-green surface with dark matrix and vitreous-to-waxy luster. Chrysocolla is typically Mohs 2–4 and noncrystalline/microcrystalline; chalcedony is Mohs 6.5–7, so hardness testing is useful.

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Physical properties

Polished/tumbled, opaque to translucent blue-green surface with dark matrix and vitreous-to-waxy luster. Chrysocolla is typically Mohs 2–4 and noncrystalline/microcrystalline; chalcedony is Mohs 6.5–7, so hardness testing is useful.

Formation & geological history

Chrysocolla forms as a secondary copper mineral in oxidized zones of copper deposits, commonly during the Cenozoic or older weathering cycles. Chalcedony forms when silica-rich groundwater fills cavities and fractures, later being colored or artificially dyed.

Uses & applications

Used primarily as a lapidary and collectible stone; attractive chrysocolla may be made into cabochons, beads, and carvings. It has little construction or industrial value.

Geological facts

Natural chrysocolla often shows blue, green, turquoise, and brown-black matrix patterns and may resemble turquoise. A uniform vivid blue color can indicate dyeing or stabilization.

Field identification & locations

Common localities include Arizona, Nevada, Chile, Peru, and the Democratic Republic of Congo. Check for copper-blue streak, softness, porous texture, and color concentration in cracks; a gemological test is needed for certainty.