
mineral
Chalcedony
Silicon Dioxide (SiO₂)
Hardness: 6.5–7 on Mohs scale; Color: Milky white, light grey, or bluish-white; Luster: Waxy to vitreous; Crystal Structure: Trigonal (cryptocrystalline); Cleavage: None; Relief: Translucent to opaque; Specific gravity: 2.58–2.64.
- Hardness
- 6
- Color
- Milky white, light grey, or bluish-white
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5–7 on Mohs scale; Color: Milky white, light grey, or bluish-white; Luster: Waxy to vitreous; Crystal Structure: Trigonal (cryptocrystalline); Cleavage: None; Relief: Translucent to opaque; Specific gravity: 2.58–2.64.
Formation & geological history
Formed through the deposition of silica-rich fluids in volcanic cavities, lava pockets, or sedimentary environments at relatively low temperatures. It often fills veins or amygdules in igneous rocks.
Uses & applications
Commonly used as a gemstone in jewelry (cabochons), as ornamental carvings, and historically for tools like arrowheads and seals. It is also used as an industrial abrasive and in precision bearings.
Geological facts
Chalcedony is a cryptocrystalline form of silica, meaning its crystals are so small they are only visible under a microscope. It includes famous varieties such as Agate, Onyx, and Carnelian.
Field identification & locations
Identify in the field by its waxy luster, lack of visible crystals, and conchoidal (shell-like) fracture. Commonly found in Brazil, India, Madagascar, and the western United States. Collectors should look for unique translucency and uniform color.
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