
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 incorrectPolished, 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.
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