
mineral
Carnelian (Orange Chalcedony)
Silicon Dioxide (SiO2)
Hardness: 6.5-7 (Mohs scale); Color: Pale orange to deep reddish-brown; Luster: Vitreous to waxy; Crystal structure: Trigonal/Hexagonal (microcrystalline/cryptocrystalline); Cleavage: None; Specific Gravity: 2.58-2.64.
- Hardness
- 6
- Color
- Pale orange to deep reddish-brown
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Pale orange to deep reddish-brown; Luster: Vitreous to waxy; Crystal structure: Trigonal/Hexagonal (microcrystalline/cryptocrystalline); Cleavage: None; Specific Gravity: 2.58-2.64.
Formation & geological history
Formed in volcanic environments and sedimentary deposits. It typically forms from the precipitation of silica from aqueous fluids in cavities (vughs) of igneous rocks or through petrification of organic matter. Its color is derived from iron oxide impurities.
Uses & applications
Primarily used as a gemstone for jewelry (cabochons, beads, and carvings), intaglio seals, and by crystal collectors for its aesthetic appeal. Historically used as a material for seal stones in ancient civilizations.
Geological facts
Ancient Romans and Greeks used carnelian for signet rings because hot wax does not stick to it. It was also one of the stones used in the Breastplate of Aaron mentioned in the Bible. It is the modern birthstone for the zodiac sign Virgo.
Field identification & locations
Identify in the field by its semi-translucency, waxy luster, and conchoidal (shell-like) fracture. Look for it in riverbeds or gravel deposits, especially in regions with volcanic history like India, Brazil, or the Pacific Northwest (USA).
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