
mineral
Carnelian (Orange Chalcedony)
Silicon Dioxide (SiO2) with iron oxide impurities
Hardness: 6.5-7 (Mohs scale); Color: Translucent orange to reddish-brown; Luster: Waxy to vitreous; Crystal Structure: Trigonal (microcrystalline/cryptocrystalline); Cleavage: None; Specific Gravity: 2.58–2.64.
- Hardness
- 6
- Color
- Translucent orange to reddish-brown
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Translucent orange to reddish-brown; Luster: Waxy to vitreous; Crystal Structure: Trigonal (microcrystalline/cryptocrystalline); Cleavage: None; Specific Gravity: 2.58–2.64.
Formation & geological history
Formed through the deposition of silica from groundwater in cavities of igneous rocks (like basalt) or sedimentary environments. The orange hue comes from hematite (iron oxide) inclusions.
Uses & applications
Extensively used as a gemstone in jewelry (cabochons), beads, and intaglios. Historically used for seal stones and amulets.
Geological facts
In ancient times, carnelian was believed to give courage in battle and help speakers become bold. It is the most famous variety of chalcedony and has been used for jewelry for over 4,500 years, appearing in Sumerian and Egyptian burials.
Field identification & locations
Identify by its translucent 'glow' when held to light, waxy luster, and lack of visible crystalline structure. Commonly found in Brazil, India, Uruguay, and Madagascar.
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