Rock Identifier
Tumbled blue-green chrysocolla (likely chrysocolla with quartz) (Chrysocolla, hydrated copper aluminum silicate; commonly intergrown with quartz, Cu₂H₂Si₂O₅(OH)₄) — mineral
mineral

Tumbled blue-green chrysocolla (likely chrysocolla with quartz)

Chrysocolla, hydrated copper aluminum silicate; commonly intergrown with quartz, Cu₂H₂Si₂O₅(OH)₄

AI-generated identification · may be incorrect

Usually blue to blue-green with pale or dark veining, vitreous to waxy luster, and opaque to translucent appearance; Mohs hardness is 2.5–3.5 for chrysocolla, higher if quartz-rich. The rounded shape indicates tumbling and polishing; crystal structure is commonly poorly crystalline or cryptocrystalline.

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Physical properties

Usually blue to blue-green with pale or dark veining, vitreous to waxy luster, and opaque to translucent appearance; Mohs hardness is 2.5–3.5 for chrysocolla, higher if quartz-rich. The rounded shape indicates tumbling and polishing; crystal structure is commonly poorly crystalline or cryptocrystalline.

Formation & geological history

Forms as a secondary copper mineral in oxidized zones above copper deposits, commonly replacing or coating host rock. It is geologically young relative to its host deposits and often occurs with malachite, azurite, limonite, and quartz.

Uses & applications

Used as a lapidary stone for cabochons, beads, carvings, and tumbled specimens; it is generally unsuitable for heavy construction because of softness and weathering sensitivity.

Geological facts

The vivid color comes from copper; blue-green chrysocolla is frequently stabilized with resin or bonded to quartz to improve durability.

Field identification & locations

Identify it by its turquoise-like blue-green color, irregular banding, softness, and association with copper minerals; common sources include Arizona, Nevada, Chile, Peru, Mexico, and the Democratic Republic of Congo.