
mineral
Carnelian Agate
Carnelian (SiO2 with iron oxide impurities)
AI-generated identification · may be incorrectHardness: 6.5-7 on Mohs scale; Color: Orange, reddish-brown, semi-translucent; Luster: Vitreous to waxy; Crystal structure: Hexagonal (trigonal microcrystalline); Cleavage: None/Conchoidal fracture; Specific gravity: 2.58-2.64.
- Hardness
- 6
- Color
- Orange, reddish-brown, semi-translucent
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Orange, reddish-brown, semi-translucent; Luster: Vitreous to waxy; Crystal structure: Hexagonal (trigonal microcrystalline); Cleavage: None/Conchoidal fracture; Specific gravity: 2.58-2.64.
Formation & geological history
Forms through the deposition of silica from groundwater into cavities of igneous rocks (volcanic lavas) or sedimentary rocks. The orange color is caused by iron oxide impurities. This process can occur over millions of years.
Uses & applications
Widely used for gemstone carvings, beads for jewelry, cabochons, and as pocket stones or talismans in the spiritual crystal market.
Geological facts
Carnelian was prized in ancient Egypt for amulets and rings, often associated with the solar disk and the goddess Isis. In ancient Rome, it was used for signet rings because hot wax does not stick to it.
Field identification & locations
Look for a translucent orange to brownish-red appearance with characteristic banded or waxy texture. It can be found in riverbeds or coastal areas where volcanic rock has weathered away. Common locations include Brazil, India, and Madagascar.
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