
mineral
Blue Chalcedony
Chalcedony (SiO2)
Hardness: 6.5-7 on Mohs scale; Color: Grayish-blue, lavender-blue; Luster: Waxy to vitreous; Crystal Structure: Microcrystalline (trigonal); Cleavage: None; Fracture: Conchoidal; Specific Gravity: 2.60-2.65.
- Hardness
- 6
- Color
- Grayish-blue, lavender-blue
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Grayish-blue, lavender-blue; Luster: Waxy to vitreous; Crystal Structure: Microcrystalline (trigonal); Cleavage: None; Fracture: Conchoidal; Specific Gravity: 2.60-2.65.
Formation & geological history
Formed by the deposition of silica from groundwater in cavities of igneous rocks such as basalt, or in sedimentary environments. Its blue color is caused by the Tyndall effect (light scattering) rather than chemical impurities.
Uses & applications
Used primarily in jewelry as cabochons or beads, ornamental carvings, and as a healing stone in holistic practices. Traditionally used as a semi-precious gemstone.
Geological facts
Chalcedony has been used for centuries to carve seals and talismans. Famous historical deposits include the 'Blue Holly' from Oregon and the high-quality deposits in Namibia (African Blue).
Field identification & locations
Identify by its waxy luster, lack of cleavage, and translucent blue-gray hue. Commonly found in Namibia, Turkey, India, and the United States (western states). Field identification often relies on its hardness and smooth, water-worn appearance when found as a pebble.
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