
mineral
Banded Agate
Cryptocrystalline variety of Quartz (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale). Color: Translucent tan, brown, and white with distinct banding. Luster: Waxy to vitreous. Crystal structure: Trigonal/Microcrystalline. Cleavage: None (Conchoidal fracture).
- Hardness
- 6
- Color
- Translucent tan, brown, and white with distinct banding
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 (Mohs scale). Color: Translucent tan, brown, and white with distinct banding. Luster: Waxy to vitreous. Crystal structure: Trigonal/Microcrystalline. Cleavage: None (Conchoidal fracture).
Formation & geological history
Formed primarily in cavities of volcanic rocks (vesicles) or metamorphic rocks by the deposition of silica from groundwater. The characteristic bands are formed by rhythmic crystallization changes over time.
Uses & applications
Widely used for lapidary arts, jewelry (cabochons), ornamental carvings, and as a semi-precious gemstone. Historically used for making precision bearings and mortars/pestles due to its hardness.
Geological facts
Agate is often named after the Achates River in Sicily where it was first discovered. The circular or parallel bands represent 'fossilized' records of the geochemical environment at the time of deposit.
Field identification & locations
Identify in the field by its translucency when held to light, smooth waxy texture when wet, and the presence of parallel concentric bands. Commonly found in riverbeds, gravel pits, and volcanic regions like the Lake Superior area.
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Epidote
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