Rock Identifier
Tumbled blue-green stone, likely chrysocolla-bearing jasper (Chrysocolla-rich chalcedony/jasper; commonly a mixture of chrysocolla (hydrated copper silicate, variable formula) and quartz (SiO₂)) — mineral
mineral

Tumbled blue-green stone, likely chrysocolla-bearing jasper

Chrysocolla-rich chalcedony/jasper; commonly a mixture of chrysocolla (hydrated copper silicate, variable formula) and quartz (SiO₂)

AI-generated identification · may be incorrect

Polished, opaque blue-green with darker mottling and a vitreous-to-waxy luster; estimated Mohs hardness 5–7 depending on quartz content, with no visible cleavage and massive microcrystalline structure.

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Physical properties

Polished, opaque blue-green with darker mottling and a vitreous-to-waxy luster; estimated Mohs hardness 5–7 depending on quartz content, with no visible cleavage and massive microcrystalline structure.

Formation & geological history

Forms in oxidized zones above copper deposits, where copper-rich fluids alter silica-bearing rock; typically Cenozoic to older, depending on the host deposit. The specimen has been shaped and polished, obscuring its original texture.

Uses & applications

Used as a decorative and lapidary material for cabochons, carvings, beads, and tumbled stones; too variable and generally too soft for high-wear jewelry.

Geological facts

Chrysocolla’s vivid color comes from hydrated copper minerals, and specimens may grade into turquoise, malachite, azurite, or quartz. Exact identification requires hardness, streak, or laboratory testing.

Field identification & locations

Commonly found in copper districts of Arizona, Nevada, Chile, Peru, Mexico, and Australia; blue-green color, opaque appearance, and copper-associated mineral patterns are useful clues. Avoid harsh chemicals and prolonged soaking if chrysocolla-rich.