
mineral
Carnelian
Carnelian (SiO2 - Silicon Dioxide)
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale); Color: Orange, red, brownish-red; Luster: Vitreous to waxy; Crystal Structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.64
- Hardness
- 6
- Color
- Orange, red, brownish-red
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Orange, red, brownish-red; Luster: Vitreous to waxy; Crystal Structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.64
Formation & geological history
Formed as a cryptocrystalline variety of chalcedony, usually in volcanic and sedimentary rocks where silica-rich fluids permeate cavities. Iron oxide impurities provide the distinct color gradient.
Uses & applications
Primarily used as a gemstone in jewelry (cabochons, beads), decorative carvings, and as a popular specimen for crystal collectors.
Geological facts
Carnelian has been used since the Neolithic period; it was highly prized in Ancient Egypt where it was believed to assist the soul in its journey to the afterlife. It was also widely used for signet rings and seals in Roman times because hot wax does not stick to it.
Field identification & locations
Identify by its translucent to semi-opaque orange-red body color and lack of banding (which distinguishes it from sardonyx or agate). Found globally in Brazil, India, Madagascar, and Uruguay. Collectors should look for even color saturation and high translucency.
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Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
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Igneous Pegmatite
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Granite
Granite (Phaneritic intrusive igneous rock)
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