mineral

Chrysocolla and Malachite Beads

Hydrated copper silicates (Chrysocolla) and Copper carbonate hydroxide (Malachite)

AI-generated identification · may be incorrect

Hardness: 2-4 (Chrysocolla) to 3.5-4 (Malachite); Color: Cyan, teal, and deep forest green; Luster: Vitreous to dull; Crystal structure: Monoclinic; Cleavage: None/Poor; Specific gravity: 2.0-2.4 (Chrysocolla) to 3.6-4.0 (Malachite)

Hardness: 2-4 (Chrysocolla) to 3
Color: Cyan, teal, and deep forest green
Luster: Vitreous to dull

Identified April 25, 2026More mineral →

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Physical properties

Formation & geological history

Formed as secondary minerals in the oxidation zones of copper ore bodies. These minerals result from the weathering of primary copper minerals by groundwater enriched with silica or carbonate.

Uses & applications

Primarily used as a semi-precious gemstone in jewelry and for lapidary carvings; historically used as a minor copper ore.

Geological facts

Chrysocolla was named by Theophrastus in 315 BCE from the Greek words for 'gold' and 'glue,' as it was used as a soldering agent for gold. Both minerals are often found intergrown, creating the unique mottled patterns seen in the beads.

Field identification & locations

Identify in the field by the distinct blue-green color near copper mines. To distinguish from imitation glass or plastic, check for coldness to the touch and natural variations in banding and inclusions.