
mineral
Carnelian (Chalcedony)
Silicon Dioxide (SiO2)
Hardness: 6.5–7 on the Mohs scale; Color: Orange-red to brownish-red; Luster: Vitreous to waxy; Crystal structure: Hexagonal/trigonal (cryptocrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.59–2.61
- Hardness
- 6
- Color
- Orange-red to brownish-red
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5–7 on the Mohs scale; Color: Orange-red to brownish-red; Luster: Vitreous to waxy; Crystal structure: Hexagonal/trigonal (cryptocrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.59–2.61
Formation & geological history
Formed in low-temperature silica-rich hydrothermal environments, often filling cavities in volcanic rocks. The red-orange color is caused by the presence of iron oxide impurities (hematite).
Uses & applications
Commonly used in jewelry as cabochons, beads, and carvings. Historically used for seals and signet rings because hot wax does not stick to it.
Geological facts
Carnelian has been used for over 4,500 years; ancient Egyptians referred to it as the 'Setting Sun' and used it in amulets for protection. It is a variety of chalcedony.
Field identification & locations
Identify by its translucent orange-red glow when held to a light source and its characteristic waxy luster. Commonly found in riverbeds and beaches where volcanic rocks have eroded.
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sedimentary
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Metamorphic
Epidote
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metamorphic
Gypsum (variety Selenite or Alabaster)
Calcium sulfate dihydrate (CaSO4·2H2O)
Mineral
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Nephrite
Mineral/Rock
Banded Gneiss (River Rock/Pebble)
Gneiss (specifically a banded variety often found as a river rock)
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