
Mineral
Carnelian
Carnelian (Microcrystalline Quartz, SiO2)
Hardness: 6.5-7 on Mohs scale; Color: Translucent orange to reddish-brown (caused by iron oxide); Luster: Vitreous to waxy; Crystal structure: Trigonal/Hexagonal (cryptocrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.58–2.64
- Hardness
- 6
- Color
- Translucent orange to reddish-brown (caused by iron oxide)
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Translucent orange to reddish-brown (caused by iron oxide); Luster: Vitreous to waxy; Crystal structure: Trigonal/Hexagonal (cryptocrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.58–2.64
Formation & geological history
Formed from the deposition of silica from groundwater in the cavities of igneous rocks such as basalt and rhyolite. It can be found in sedimentary environments where volcanic rocks have eroded. It does not have a specific 'age' but is found in prehistoric to recent deposits.
Uses & applications
Primarily used as a gemstone for jewelry (cabochons, beads, and cameos) and ornamental carvings. It is also highly valued in the metaphysical and crystal collecting community.
Geological facts
Carnelian has been used for over 4,500 years; ancient Egyptians called it 'the setting sun' and buried their dead with it to help them in the afterlife. It was also used for cylinder seals in Mesopotamia and signet rings in ancient Rome.
Field identification & locations
Identify in the field by its distinct orange translucency, waxy feel, and conchoidal (shell-like) fracture patterns. It is commonly found in India, Brazil, Egypt, Uruguay, and the United States (notably Washington and Oregon). Collectors should look for even color and high translucency.
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