Rock Identifier
Polished chrysocolla-bearing copper mineral specimen (Chrysocolla, Cu₂H₂Si₂O₅(OH)₄·nH₂O, likely mixed with malachite and limonite/goethite) — mineral
mineral

Polished chrysocolla-bearing copper mineral specimen

Chrysocolla, Cu₂H₂Si₂O₅(OH)₄·nH₂O, likely mixed with malachite and limonite/goethite

AI-generated identification · may be incorrect

Blue-green, yellow-green, brown and rusty-red mottling with a glossy polished surface; typically opaque, botryoidal or massive, amorphous to microcrystalline. Chrysocolla hardness is about 2.5–3.5 Mohs; specific gravity approximately 1.9–2.3. Brown areas may be iron oxides, while green zones may include malachite.

Identified More mineral
Explore Polished chrysocolla-bearing copper mineral specimen in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

Blue-green, yellow-green, brown and rusty-red mottling with a glossy polished surface; typically opaque, botryoidal or massive, amorphous to microcrystalline. Chrysocolla hardness is about 2.5–3.5 Mohs; specific gravity approximately 1.9–2.3. Brown areas may be iron oxides, while green zones may include malachite.

Formation & geological history

Forms in oxidized zones above copper-ore deposits when copper-bearing fluids react with silica-rich groundwater. It is generally a secondary mineral, commonly associated with malachite, azurite, quartz, and limonite; the specimen’s exact age cannot be determined from the photograph.

Uses & applications

Used mainly as a lapidary and collector material for cabochons, polished slices, and display specimens; its softness makes it unsuitable for most everyday jewelry. Not generally used as an industrial copper ore unless copper minerals are concentrated.

Geological facts

The vivid blue-green color is characteristic of hydrated copper silicate, but polished mixed material is often sold as “chrysocolla matrix.” The surface appears resin-glossy, so it may be stabilized or coated.

Field identification & locations

Commonly found in copper districts such as Arizona, Chile, Peru, the Democratic Republic of Congo, and Australia. Confirm with hardness, streak, and copper-mineral associations; regional occurrence near 45.5°N, 16.4°E is possible but not especially diagnostic, so the locality cannot be inferred confidently.