
mineral
Banded Agate
Cryptocrystalline Quartz (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 Mohs; Color: Brown, tan, and white concentric banding; Luster: Waxy to vitreous; Crystal Structure: Hexagonal (cryptocrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.64
- Hardness
- 6
- Color
- Brown, tan, and white concentric banding
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 Mohs; Color: Brown, tan, and white concentric banding; Luster: Waxy to vitreous; Crystal Structure: Hexagonal (cryptocrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.64
Formation & geological history
Formed through the deposition of silica from groundwater into cavities (vesicles) in igneous rocks, specifically volcanic lavas. The banding represents pulse-like deposition cycles over thousands of years.
Uses & applications
Used primarily for jewelry (cabochons, beads), decorative carvings, and as pocket stones. Historically used for making mortar and pestles due to its hardness and resistance to chemicals.
Geological facts
The distinct bands are often thinner than a human hair. No two agates are identical, making them favorites for collectors. Agates have been used in amulets and jewelry since the time of Ancient Babylon.
Field identification & locations
Identify by its characteristic waxy luster and distinct parallel or concentric bands. It is frequently found in riverbeds, shorelines (like the Great Lakes), and volcanic regions. It will scratch glass but cannot be scratched by a steel knife.
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