Rock Identifier
Tumbled chrysocolla beads (Chrysocolla, hydrated copper-aluminum silicate (approximately (Cu,Al)₂H₂Si₂O₅(OH)₄·nH₂O), commonly mixed with malachite or quartz) — mineral
mineral

Tumbled chrysocolla beads

Chrysocolla, hydrated copper-aluminum silicate (approximately (Cu,Al)₂H₂Si₂O₅(OH)₄·nH₂O), commonly mixed with malachite or quartz

AI-generated identification · may be incorrect

Typically blue-green to teal with mottled black, brown, or green patterns; vitreous to waxy luster; amorphous or cryptocrystalline; hardness about 2.5–3.5 Mohs, sometimes higher when quartz-rich; no obvious cleavage. The pictured material is polished into beads and may be stabilized or resin-treated.

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Physical properties

Typically blue-green to teal with mottled black, brown, or green patterns; vitreous to waxy luster; amorphous or cryptocrystalline; hardness about 2.5–3.5 Mohs, sometimes higher when quartz-rich; no obvious cleavage. The pictured material is polished into beads and may be stabilized or resin-treated.

Formation & geological history

Forms as a secondary copper mineral in oxidized zones of copper deposits, commonly alongside malachite, azurite, limonite, and quartz. It ranges from young weathering-zone material to deposits of considerable geological age.

Uses & applications

Used for beads, cabochons, carvings, and decorative objects; rarely used industrially because it is soft and often porous.

Geological facts

Its vivid color comes from copper; “gem chrysocolla” is generally quartz-rich and more durable than ordinary chrysocolla.

Field identification & locations

Identify by its blue-green color, low hardness, mottled appearance, and association with copper minerals; common sources include Arizona, Nevada, Chile, Peru, Mexico, and the Democratic Republic of Congo. Avoid harsh chemicals and prolonged soaking.