
Mineral
Banded Agate (Jasper-Agate)
Silicon Dioxide (SiO₂)
Hardness: 6.5–7 on the Mohs scale. Color: Brown, red, and white/gray banding. Luster: Vitreous to waxy. Crystal structure: Cryptocrystalline (Trigonal). Cleavage: None (Conchoidal fracture). Specific Gravity: 2.60–2.65.
- Hardness
- 6
- Color
- Brown, red, and white/gray banding
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5–7 on the Mohs scale. Color: Brown, red, and white/gray banding. Luster: Vitreous to waxy. Crystal structure: Cryptocrystalline (Trigonal). Cleavage: None (Conchoidal fracture). Specific Gravity: 2.60–2.65.
Formation & geological history
Formed through the deposition of silica from groundwater into the cavities of igneous rocks such as basalt or rhyolite. The banding results from rhythmic crystallization over thousands of years. Often found in volcanic ash beds or sedimentary deposits.
Uses & applications
Primarily used for lapidary arts, jewelry (cabochons), interior decoration, and as architectural accents. Historically used for making hardstone cameos and amulets.
Geological facts
Agate belongs to the chalcedony family. The distinct bands are caused by different mineral impurities (like iron or manganese oxide) entering the solution during formation. It was named by Theophrastus after the Achates River in Sicily.
Field identification & locations
Identify in the field by its distinct waxy luster and translucent to opaque concentric banding. Often found along riverbeds, beaches, or in volcanic terrains. Tips for collectors: Look for high color contrast and lack of fractures; common in areas like Lake Superior (USA), Brazil, and India.
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