
gemstone
Chrysoprase
Chalcedony (SiO2)
AI-generated identification · may be incorrectHardness: 6.5 to 7 on the Mohs scale; Color: Apple green to dark green; Luster: Vitreous to waxy; Crystal structure: Microcrystalline quartz (trigonal); Cleavage: None, exhibits conchoidal fracture; Specific gravity: 2.58 to 2.62
- Hardness
- 6
- Color
- Apple green to dark green
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5 to 7 on the Mohs scale; Color: Apple green to dark green; Luster: Vitreous to waxy; Crystal structure: Microcrystalline quartz (trigonal); Cleavage: None, exhibits conchoidal fracture; Specific gravity: 2.58 to 2.62
Formation & geological history
Formed by the secondary weathering or hydrothermal alteration of nickel-bearing serpentinites or other ultramafic rocks, where silica-rich groundwater interacts with nickel minerals.
Uses & applications
Used primarily as a semi-precious gemstone in jewelry, for carvings, beads, and ornamental objects.
Geological facts
Chrysoprase gets its distinct apple-green color from trace amounts of nickel rather than chromium or vanadium. It was highly prized by the ancient Greeks, Romans, and Egyptians for use in signet rings and decorative carvings.
Field identification & locations
Can be identified in the field by its waxy luster, conchoidal fracture, and characteristic bright apple-green coloration. Commonly found in Australia, Germany, Poland, Russia, Arizona, and California.
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