
mineral
Blue Chalcedony
Chalcedony (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale); Color: Pale blue, lavender-blue, or grayish-blue; Luster: Waxy to vitreous; Crystal structure: Hexagonal (trigonal) cryptocrystalline; Cleavage: None; Specific gravity: 2.58-2.64
- Hardness
- 6
- Color
- Pale blue, lavender-blue, or grayish-blue
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Pale blue, lavender-blue, or grayish-blue; Luster: Waxy to vitreous; Crystal structure: Hexagonal (trigonal) cryptocrystalline; Cleavage: None; Specific gravity: 2.58-2.64
Formation & geological history
Formed through the deposition of silica from aqueous solutions in cavities of volcanic rocks (basalts) and sedimentary environments at relatively low temperatures.
Uses & applications
Primarily used as a gemstone in jewelry (cabochons, beads), decorative carvings, and as a popular specimen for mineral collectors.
Geological facts
Chalcedony was named after the ancient Greek town of Chalkedon in Asia Minor. It is a cryptocrystalline form of silica, meaning its crystals are too small to be seen without high magnification.
Field identification & locations
Identify in the field by its waxy luster, conchoidal fracture (smooth, curved breaks), and hardness (it will scratch glass). It is commonly found in Malawi, Namibia, Turkey, and various locations in the SW United States.
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Epidote
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