
mineral
Agate (Fortification Agate)
Banded Chalcedony (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7. Color: White, cream, and tan with distinct banding. Luster: Waxy to vitreous. Crystal structure: Cryptocrystalline. Cleavage: None (conchoidal fracture). Specific Gravity: 2.58-2.64.
- Hardness
- 6
- Color
- White, cream, and tan with distinct banding
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7. Color: White, cream, and tan with distinct banding. Luster: Waxy to vitreous. Crystal structure: Cryptocrystalline. Cleavage: None (conchoidal fracture). Specific Gravity: 2.58-2.64.
Formation & geological history
Formed as a secondary mineral in the cavities (vesicles) of volcanic rocks (igneous) through the deposition of silica-rich groundwater. The layers form sequentially over thousands of years.
Uses & applications
Used primarily for lapidary work, jewelry (cabochons), or as a collector's specimen. Known for being durable and taking a high polish.
Geological facts
The 'V-shaped' lines visible in this specimen are known as 'fortification' banding because they resemble the floor plans of old star-shaped fortresses. Agate has been used for ornaments since Ancient Greek times.
Field identification & locations
Identify by looking for translucent edges, waxy luster, and concentric or angular banding. This specimen appears to be a fragment showing a conchoidal fracture. Commonly found in riverbeds or volcanic outcrop areas.
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