
mineral
Chalcedony (Agate)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 on Mohs scale; Color: Grayish-blue, translucent to opaque; Luster: Waxy to vitreous; Crystal Structure: Cryptocrystalline (Trigonal/Monoclinic); Cleavage: None; Specific Gravity: 2.58-2.64.
- Hardness
- 6
- Color
- Grayish-blue, translucent to opaque
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Grayish-blue, translucent to opaque; Luster: Waxy to vitreous; Crystal Structure: Cryptocrystalline (Trigonal/Monoclinic); Cleavage: None; Specific Gravity: 2.58-2.64.
Formation & geological history
Formed through the deposition of silica-rich fluids in volcanic cavities (vesicles) or sedimentary rock fractures. Often found in basalt flows or as nodules in limestone.
Uses & applications
Used primarily in lapidary arts for jewelry, cabochons, and decorative carvings. Historically used for making tools due to its conchoidal fracture and hardness.
Geological facts
Chalcedony is a cryptocrystalline form of silica, meaning its crystals are so small they can only be seen under high magnification. It is a family that includes carnelian, onyx, and agate.
Field identification & locations
Identify in the field by its waxy luster, conchoidal (shell-like) fracture, and translucent edges when held to light. Common in river beds, beaches, and volcanic regions.
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Sandstone (with potential mineral staining/concretions)
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Epidote
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Granite
Granite (Phaneritic intrusive igneous rock)
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