
mineral
Blue Chalcedony
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs); Color: Pale blue, lavender-blue, or grey-blue; Luster: Waxy to vitreous; Crystal Structure: Trigonal (microcrystalline); Cleavage: None; Specific Gravity: 2.60-2.65
- Hardness
- 6
- Color
- Pale blue, lavender-blue, or grey-blue
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 (Mohs); Color: Pale blue, lavender-blue, or grey-blue; Luster: Waxy to vitreous; Crystal Structure: Trigonal (microcrystalline); Cleavage: None; Specific Gravity: 2.60-2.65
Formation & geological history
Formed in volcanic and sedimentary environments through the deposition of silica from hydrothermal fluids or groundwater at relatively low temperatures. Often found in cavities of igneous rocks.
Uses & applications
Predominantly used as a gemstone for jewelry (cabochons, beads), decorative carvings, and as a popular specimen for crystal healing and mineral collectors.
Geological facts
Chalcedony is a cryptocrystalline form of silica, meaning its crystals are too small to be seen without high magnification. The blue variety is prized for its serene color and translucency.
Field identification & locations
Identify by its waxy luster, lack of visible crystals, and conchoidal fracture. Often found in pockets of basalts or as nodules. Common locations include Namibia, Turkey, India, and the United States (Oregon).
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