
sedimentary
Banded Calcite (often sold as 'Green Onyx')
Calcite (Calcium Carbonate, CaCO3)
AI-generated identification · may be incorrectHardness: 3 on Mohs scale (can be scratched by a copper coin); Color: Pale green to white with brown/red banding; Luster: Vitreous to waxy; Crystal structure: Trigonal; Cleavage: Perfect rhombohedral; Specific gravity: 2.71
- Hardness
- 3 on Mohs scale (can be scratched by a copper coin)
- Color
- Pale green to white with brown/red banding
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 3 on Mohs scale (can be scratched by a copper coin); Color: Pale green to white with brown/red banding; Luster: Vitreous to waxy; Crystal structure: Trigonal; Cleavage: Perfect rhombohedral; Specific gravity: 2.71
Formation & geological history
Formed through the precipitation of calcium carbonate from cold water springs or in caves as flowstone/travertine. It is relatively young in geological terms, often forming in the Quaternary period.
Uses & applications
Primarily used for decorative carvings, figurines, bookends, and low-cost jewelry. It is a popular material for ornamental stone craft due to its softness and translucency.
Geological facts
Despite being called 'Green Onyx' in the trade, it is not true onyx (which is a form of cryptocrystalline quartz). True onyx is much harder (Mohs 7), whereas this calcite is soft and will react/fizz if it comes into contact with even weak acids like vinegar.
Field identification & locations
Identify in the field by its softness (easily scratched by a steel blade) and its characteristic light-to-dark parallel banding. It is commonly found in Mexico, Pakistan, and Iran.
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