
mineral
Carnelian (a variety of Chalcedony)
Silicon Dioxide (SiO2) with iron oxide impurities
Hardness: 6.5–7 on the Mohs scale. Color: Translucent reddish-brown to orange. Luster: Vitreous to waxy. Crystal Structure: Hexagonal (Trigonal), specifically microcrystalline. Cleavage: None (conchoidal fracture). Specific Gravity: 2.58–2.64.
- Hardness
- 6
- Color
- Translucent reddish-brown to orange
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5–7 on the Mohs scale. Color: Translucent reddish-brown to orange. Luster: Vitreous to waxy. Crystal Structure: Hexagonal (Trigonal), specifically microcrystalline. Cleavage: None (conchoidal fracture). Specific Gravity: 2.58–2.64.
Formation & geological history
Formed in volcanic cavities or sedimentary environments through the deposition of silica-rich groundwater. Its reddish color comes from hematite (iron oxide) impurities during the crystallization process. It can be found in various age deposits, from ancient volcanic host rocks to modern river beds.
Uses & applications
Mostly used in jewelry (beads, cabochons, carved intaglios), spiritual healing/gemstone collecting, and historical ornamentation. Its durability makes it suitable for rings and pendants.
Geological facts
Carnelian was highly prized in ancient times; it was used for seal stones in ancient Egypt and Rome because hot wax does not stick to it. It is the birthstone for the zodiac sign of Virgo and represented the setting sun to ancient Egyptians.
Field identification & locations
Identify by its translucent warm orange-red color and waxy surface. Look for it in river gravels, desert plains, or near volcanic regions like the Lake Superior area (as Lake Superior Agate relative) or India. For collectors, use a flashlight to check for translucency; simple quartz will be more opaque or colorless.
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