
mineral
Carnelian
Carnelian (SiO2 with Iron Oxide impurities)
Hardness: 6.5-7 on Mohs scale; Color: Orangey-red to brownish-red; Luster: Waxy to vitreous; Crystal Structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.64.
- Hardness
- 6
- Color
- Orangey-red to brownish-red
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Orangey-red to brownish-red; Luster: Waxy to vitreous; Crystal Structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.64.
Formation & geological history
Formed by the deposition of silica from groundwater into cavities of igneous rocks. The red color is caused by the presence of iron oxide (hematite) through oxidation over geological periods.
Uses & applications
Primarily used as a gemstone in jewelry (cabochons, beads, and rings) and for lapidary art such as seals and talismans. Occasionally used in ornamental carvings.
Geological facts
In ancient times, carnelian was believed to protect the wearer and was buried with Egyptian pharaohs. It was also used for signet rings because hot wax does not stick to it.
Field identification & locations
Identify by its translucent, waxy appearance and warm reddish-orange hue. In the field, look for nodules in sedimentary rocks or volcanic areas. Common locations include Brazil, India, Madagascar, and Uruguay.
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