
mineral
Carnelian
Silicon Dioxide (Quartz variety, SiO2)
AI-generated identification · may be incorrectHardness: 6.5 to 7 on the Mohs scale. Color: Orange, reddish-orange, brownish-orange, or red. Luster: Vitreous to waxy. Crystal structure: Trigonal (microcrystalline quartz/chalcedony). Cleavage: None, exhibits conchoidal fracture. Specific gravity: 2.58 to 2.64.
- Hardness
- 6
- Color
- Orange, reddish-orange, brownish-orange, or red
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5 to 7 on the Mohs scale. Color: Orange, reddish-orange, brownish-orange, or red. Luster: Vitreous to waxy. Crystal structure: Trigonal (microcrystalline quartz/chalcedony). Cleavage: None, exhibits conchoidal fracture. Specific gravity: 2.58 to 2.64.
Formation & geological history
Formed in low-temperature environments, typically as groundwater deposits in cavities of volcanic rocks or sedimentary deposits where silica-rich solutions precipitate. Geological age varies widely depending on the host rock, often from Mesozoic or Cenozoic volcanic activity.
Uses & applications
Used extensively in jewelry for rings, necklaces, beads, and cabochons. Historically popular for carved seals, signet rings, and talismans due to wax not sticking to its surface.
Geological facts
Carnelian was highly prized in ancient civilizations including Ancient Egypt, where it was associated with the goddess Isis and used in amulets to ensure safe passage to the afterlife. King Tutankhamun's burial mask and jewelry feature prominent carnelian inlays.
Field identification & locations
Easily identified by its translucent orange-to-red color and waxy luster with conchoidal fracture. Commonly found worldwide, notably in India, Brazil, Uruguay, Madagascar, and the United States.
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