
mineral
Carnelian Agate
Silicon Dioxide (SiO2) with high Iron Oxide impurities
AI-generated identification · may be incorrectHardness: 6.5–7 (Mohs scale); Color: Orange, reddish-brown, or deep red; Luster: Vitreous to waxy; Crystal Structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58–2.64
- Hardness
- 6
- Color
- Orange, reddish-brown, or deep red
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5–7 (Mohs scale); Color: Orange, reddish-brown, or deep red; Luster: Vitreous to waxy; Crystal Structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58–2.64
Formation & geological history
Formed from the deposition of silica from groundwater in cavities of igneous rocks. The color is derived from iron oxide impurities that have been heated over geological time.
Uses & applications
Predominantly used in jewelry, beadwork, and cabochons. Historically used for cylinder seals and signet rings because hot wax does not stick to it.
Geological facts
Ancient Romans and Greeks used carnelian for intaglio rings. It was believed to provide courage in battle and is often associated with the 'Solar Plexus' chakra in metaphysical traditions.
Field identification & locations
Identify by its translucent orange/red color and characteristic curved (conchoidal) fracture. In the field, look for pebbles with a waxy exterior in riverbeds or volcanic regions like Brazil, India, or Madagascar.
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Epidote
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Granite
Granite (Phaneritic intrusive igneous rock)
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