
mineral
Blue Chalcedony
Silicon Dioxide (SiO2) - Microcrystalline Quartz
AI-generated identification · may be incorrectHardness: 6.5–7 (Mohs); Color: Waxy translucent blue; Luster: Vitreous to waxy; Crystal structure: Trigonal (cryptocrystalline); Cleavage: None; SG: 2.58–2.64.
- Hardness
- 6
- Color
- Waxy translucent blue
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5–7 (Mohs); Color: Waxy translucent blue; Luster: Vitreous to waxy; Crystal structure: Trigonal (cryptocrystalline); Cleavage: None; SG: 2.58–2.64.
Formation & geological history
Formed in low-temperature hydrothermal environments where silica-rich fluids deposit in cavities of volcanic and sedimentary rocks. Common in basaltic geodes.
Uses & applications
Used primarily in jewelry as cabochons, lapidary carvings, beadwork, and by mineral collectors for its aesthetic translucency.
Geological facts
Its name is derived from the ancient Greek town Chalcedon. Unlike crystalline quartz (like amethyst), chalcedony is made of microscopic interlocking fibers of quartz and moganite.
Field identification & locations
Identify by its waxy luster, conchoidal fracture, and lack of visible crystal faces. Found commonly in Brazil, Namibia, Turkey, and the USA (Oregon/California).
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Septarian Pebble
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