
mineral
Carnelian
Carnelian (SiO2 with iron oxide impurities)
Hardness: 6.5-7 on Mohs scale; Color: Reddish-orange to brownish-red; Luster: Vitreous to waxy; Crystal structure: Trigonal/Cryptocrystalline; Specific Gravity: 2.59-2.61. This specimen is polished and translucent.
- Hardness
- 6
- Color
- Reddish-orange to brownish-red
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Reddish-orange to brownish-red; Luster: Vitreous to waxy; Crystal structure: Trigonal/Cryptocrystalline; Specific Gravity: 2.59-2.61. This specimen is polished and translucent.
Formation & geological history
Formed by the precipitation of silica from groundwater into cavities of igneous rocks, particularly volcanic lavas. The reddish color is due to iron oxide (hematite) impurities and can be enhanced by heat treatment.
Uses & applications
Widely used for centuries in jewelry, beadwork, seals, cabochons, and as a decorative collector's stone. In ancient times, it was popular for signet rings and amulets.
Geological facts
Ancient Egyptians called carnelian 'the setting sun' or 'the blood of Isis.' It was believed to provide courage and protection in the afterlife. It is the red variety of Chalcedony.
Field identification & locations
Identified by its waxy luster, lack of visible crystals (cryptocrystalline), and its distinct orange-red translucency. Commonly found in Brazil, India, Uruguay, Madagascar, and the United States.
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