
mineral
Carnelian
Chalcedony (SiO2) with Iron Oxide inclusions
AI-generated identification · may be incorrectHardness: 6.5-7.0 (Mohs); Color: Orange, reddish-brown, brownish; Luster: Vitreous to waxy; Crystal structure: Trigonal/Microcrystalline; Cleavage: None; Fracture: Conchoidal; Specific Gravity: 2.58-2.64
- Hardness
- 6
- Color
- Orange, reddish-brown, brownish
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5-7.0 (Mohs); Color: Orange, reddish-brown, brownish; Luster: Vitreous to waxy; Crystal structure: Trigonal/Microcrystalline; Cleavage: None; Fracture: Conchoidal; Specific Gravity: 2.58-2.64
Formation & geological history
Formed in low-temperature silica-rich environments, often in volcanic rock cavities or sedimentary geodes. The color is derived from iron oxide impurities (hematite).
Uses & applications
Primarily used as a gemstone for jewelry (cabochons, beads), decorative carvings, and in alternative healing practices (metaphysical crystals).
Geological facts
Carnelian has been used for over 4,500 years; ancient Romans used it to make seal rings and signets because hot wax does not stick to it.
Field identification & locations
Identify by its translucent reddish-orange hue and waxy surface. Found globally with major deposits in Brazil, India, Uruguay, and Madagascar. Look for it in river beds or areas with volcanic activity.
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