
mineral
Blue Chalcedony
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 on Mohs scale. Color: Pale blue, lavender-blue, or grey-blue. Luster: Waxy to vitreous. Crystal Structure: Trigonal (microcrystalline/cryptocrystalline). Cleavage: None. Specific Gravity: 2.6-2.64.
- Hardness
- 6
- Color
- Pale blue, lavender-blue, or grey-blue
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 on Mohs scale. Color: Pale blue, lavender-blue, or grey-blue. Luster: Waxy to vitreous. Crystal Structure: Trigonal (microcrystalline/cryptocrystalline). Cleavage: None. Specific Gravity: 2.6-2.64.
Formation & geological history
Formed through the deposition of silica-rich water in volcanic cavities or sedimentary rock fractures. It is an authigenic mineral often found in hydrothermal veins and geodes.
Uses & applications
Used primarily in lapidary work for cabochons, beads, and carvings. Also used as a healing stone in metaphysical practices and as a collector's specimen.
Geological facts
Chalcedony is a cryptocrystalline form of silica, composed of very fine intergrowths of quartz and moganite. The blue color is due to the Tyndall effect, which is the scattering of light by microscopic particles.
Field identification & locations
Identify in the field by its waxy luster, conchoidal fracture, and lack of visible crystals. It is frequently found in basaltic rocks or as nodules in desert environments like those in Namibia or Turkey.
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