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

Weathered copper-bearing rock, likely chrysocolla-bearing limonite

Chrysocolla (Cu₂H₂Si₂O₅(OH)₄·nH₂O) with limonite/goethite and possibly malachite

AI-generated identification · may be incorrect

Blue-green to turquoise earthy coatings and pits occur in a brown, porous iron-oxide matrix; typically dull to waxy, amorphous, with hardness about 2–4 (chrysocolla) and specific gravity roughly 2.0–4.3. The rounded form and heavy weathering obscure the original host rock.

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Physical properties

Blue-green to turquoise earthy coatings and pits occur in a brown, porous iron-oxide matrix; typically dull to waxy, amorphous, with hardness about 2–4 (chrysocolla) and specific gravity roughly 2.0–4.3. The rounded form and heavy weathering obscure the original host rock.

Formation & geological history

Forms in the oxidized zone of copper deposits when copper-rich fluids alter silicate and iron-bearing minerals, commonly during weathering over millions of years. Exact age and locality cannot be determined from the photograph.

Uses & applications

Attractive material may be cut or polished for cabochons and specimens; copper-oxide ore zones are economically important for copper mining. This rough piece is mainly a collector specimen.

Geological facts

The green-blue color is characteristic of hydrated copper minerals, but visual identification cannot reliably distinguish chrysocolla from malachite, turquoise, or copper-bearing clay without testing.

Field identification & locations

Look for blue-green earthy color, porous iron staining, and association with copper oxides; a streak, hardness, acid, specific-gravity, or laboratory analysis would improve identification. Common localities include Arizona, Nevada, Chile, Peru, and the Democratic Republic of Congo.