
mineral
Chrysocolla in Cuprite (Sonoran Sunrise)
Cu2-xAlx(H2-xSi2O5)(OH)4·n(H2O) (Chrysocolla) and Cu2O (Cuprite)
AI-generated identification · may be incorrectHardness: 2-4 (Chrysocolla) to 3.5-4 (Cuprite); Color: Cyan blue and dark reddish-brown/black; Luster: Vitreous to dull; Crystal Structure: Amorphous/Orthorhombic (Chrysocolla) and Isometric (Cuprite); Cleavage: None/Conchoidal fracture.
- Hardness
- 2-4 (Chrysocolla) to 3
- Color
- Cyan blue and dark reddish-brown/black
- Luster
- Vitreous to dull
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Physical properties
Hardness: 2-4 (Chrysocolla) to 3.5-4 (Cuprite); Color: Cyan blue and dark reddish-brown/black; Luster: Vitreous to dull; Crystal Structure: Amorphous/Orthorhombic (Chrysocolla) and Isometric (Cuprite); Cleavage: None/Conchoidal fracture.
Formation & geological history
Secondary mineral formed in the oxidation zones of copper ore bodies. It occurs as a result of water interacting with copper minerals and silica in arid environments. Often found in deposits dating back to the Proterozoic to Cenozoic eras.
Uses & applications
Predominantly used as a gemstone for jewelry (cabochons), lapidary art, and as a collector's specimen. It is also a minor ore of copper.
Geological facts
This specific combination from Mexico is often marketed as 'Sonoran Sunrise' or 'Sonoran Sunset'. It is valued for the striking contrast between the bright blue-green chrysocolla and the deep red or black cuprite/tenorite matrix.
Field identification & locations
Identify in the field by its distinct 'bullseye' or mottled blue-on-red pattern and association with other copper minerals like Malachite. Found primarily in Sonora, Mexico, and copper mines in Arizona, USA. Collectors look for high contrast and lack of fractures.
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