
Mineral
Carnelian Agate
Silicon Dioxide (SiO2) with iron oxide impurities
Hardness: 6.5-7 on Mohs scale. Color: Translucent orange to reddish-brown. Luster: Waxy to vitreous. Crystal structure: Trigonal (microcrystalline/cryptocrystalline). Cleavage: None (conchoidal fracture). Specific gravity: 2.58-2.64.
- Hardness
- 6
- Color
- Translucent orange to reddish-brown
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 on Mohs scale. Color: Translucent orange to reddish-brown. Luster: Waxy to vitreous. Crystal structure: Trigonal (microcrystalline/cryptocrystalline). Cleavage: None (conchoidal fracture). Specific gravity: 2.58-2.64.
Formation & geological history
Formed by the deposition of silica from groundwater in cavities of igneous rocks such as basalt. The orange color is derived from iron oxide (hematite) impurities. Most specimens are prehistoric to millions of years old.
Uses & applications
Commonly used in jewelry (beads, cabochons), carvings, stone seals, and as a popular semi-precious gemstone for mineral collectors and metaphysical practitioners.
Geological facts
Carnelian has been used as a gemstone for over 4,500 years; Ancient Egyptians called it 'the setting sun' and buried their dead with it to help the soul pass into the afterlife.
Field identification & locations
Identify in the field by its distinctive orange translucency, waxy texture, and conchoidal (shell-like) fracture. Found frequently in riverbeds or coastal areas in India, Brazil, Uruguay, and the United States (especially the Pacific Northwest).
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