
mineral
Carnelian (a variety of Chalcedony)
Silicon dioxide (SiO2) with iron oxide impurities
Hardness: 6.5–7 (Mohs scale); Color: Orange to reddish-brown; Luster: Vitreous to waxy; Crystal structure: Trigonal/Microcrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.58–2.64
- Hardness
- 6
- Color
- Orange to reddish-brown
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5–7 (Mohs scale); Color: Orange to reddish-brown; Luster: Vitreous to waxy; Crystal structure: Trigonal/Microcrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.58–2.64
Formation & geological history
Formed through the deposition of silica from groundwater into cavities of igneous rocks, particularly volcanic lavas. The reddish hue is caused by iron oxide (hematite) inclusions. It can be found in formations ranging from ancient Precambrian to relatively recent volcanic deposits.
Uses & applications
Predominantly used as a gemstone for jewelry (cabochons, beads), decorative carvings, and seal stones. Historically used for signet rings and amulets.
Geological facts
Ancient Egyptians called carnelian 'the setting sun' and believed it had protective powers. It was one of the first gemstones used in bead making and was frequently used by Romans for wax seal impressions because hot wax does not stick to it.
Field identification & locations
Identify by its translucent orange-red glow when held to a light source and its smooth, waxy texture. It is commonly found in riverbeds or beaches where volcanic rocks have weathered down. Major sources include Brazil, India, Uruguay, and Madagascar.
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