
mineral
Banded Agate (specifically Black Sardonyx/Onyx variety)
Silicon Dioxide (SiO2) - Cryptocrystalline Quartz
AI-generated identification · may be incorrectHardness: 6.5-7 on the Mohs scale. Color: Alternating bands of black, grey, and white. Luster: Vitreous to waxy. Crystal Structure: Trigonal (microcrystalline). Cleavage: None. Specific Gravity: 2.60-2.65.
- Hardness
- 6
- Color
- Alternating bands of black, grey, and white
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5-7 on the Mohs scale. Color: Alternating bands of black, grey, and white. Luster: Vitreous to waxy. Crystal Structure: Trigonal (microcrystalline). Cleavage: None. Specific Gravity: 2.60-2.65.
Formation & geological history
Formed through the deposition of silica from groundwater in the cavities of igneous rocks, particularly volcanic lavas. The banding is created by rhythmic crystallization over thousands of years.
Uses & applications
Primarily used for ornamental purposes, jewelry (pendants and rings), sculptures, bookends, and collection specimens. Historically used for making cameos and intaglios.
Geological facts
This specimen features a druzy quartz center, where larger crystals grew into the open pocket of the geode. Agates were named by the Greek philosopher Theophrastus who found them along the Achates River in Sicily.
Field identification & locations
Identify by its characteristic parallel, concentric banding and waxy texture. In the field, look for nodules with a rough, weathered exterior but translucent/banded interior when cracked or cut. Commonly found in Brazil, India, and Germany.
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