
sedimentary
Banded Calcite (often sold as 'Onyx Marble' or 'Mexican Onyx')
Calcite (CaCO3) / Travertine
AI-generated identification · may be incorrectHardness: 3 on the Mohs scale; Color: Cream, tan, brown, and reddish-brown concentric bands; Luster: Vitreous to resinous (high polish); Cleavage: Perfect rhombohedral in raw crystal form; Specific Gravity: ~2.71
- Hardness
- 3 on the Mohs scale
- Color
- Cream, tan, brown, and reddish-brown concentric bands
- Luster
- Vitreous to resinous (high polish)
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Physical properties
Hardness: 3 on the Mohs scale; Color: Cream, tan, brown, and reddish-brown concentric bands; Luster: Vitreous to resinous (high polish); Cleavage: Perfect rhombohedral in raw crystal form; Specific Gravity: ~2.71
Formation & geological history
Formed chemically by the precipitation of calcium carbonate from hot springs, geothermal waters, or cave environments (flowstone/travertine), resulting in distinct rhythmic banding layers over time.
Uses & applications
Commonly carved and polished into ornamental decorative objects such as eggs, spheres, bowls, vases, and tiles. Due to low hardness, it is not suitable for faceted jewelry rings.
Geological facts
Although trade names often refer to this material as 'onyx' or 'green/red onyx,' true onyx is a cryptocrystalline variety of quartz (silicon dioxide, Mohs 7). Banded calcite is much softer (Mohs 3) and will effervesce (fizz) vigorously in dilute hydrochloric or warm vinegar.
Field identification & locations
Easily identified by its distinct banded layers, relatively soft surface (scratches easily with a copper penny or steel blade), and reaction to weak acid. Highly common in Mexico, Pakistan, Turkey, and Italy.
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