
mineral
Carnelian (Chalcedony)
Silicon Dioxide (SiO2) with Iron Oxide impurities
Hardness: 6.5-7 (Mohs scale); Color: Translucent orange to reddish-brown; Luster: Vitreous to waxy; Crystal structure: Hexagonal (microcrystalline); Cleavage: None; Fracture: Conchoidal.
- Hardness
- 6
- Color
- Translucent orange to reddish-brown
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Translucent orange to reddish-brown; Luster: Vitreous to waxy; Crystal structure: Hexagonal (microcrystalline); Cleavage: None; Fracture: Conchoidal.
Formation & geological history
Forms in pockets of volcanic rock, where silica-rich groundwater deposits minerals over time. Its color is derived from iron oxide (hematite) impurities. Often found as water-worn pebbles in stream beds.
Uses & applications
Used primarily in lapidary work, jewelry (beads, cabochons), and as a collector's stone. Historically used for signet rings and wax seals because hot wax does not stick to it.
Geological facts
Carnelian was revered by ancient Egyptians as the 'setting sun' and was mentioned as a protective stone for the heart. It is one of the oldest gemstones recorded in history, dating back to the Neolithic period.
Field identification & locations
Identify by its translucent, waxy appearance and orange color range. Found commonly in Brazil, India, Uruguay, and Madagascar. In the field, look for smooth, rounded pebbles that appear glowing or translucent when held to the light.
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