
mineral
Carnelian Agate
Silicon Dioxide (SiO2) - variety of Chalcedony
AI-generated identification · may be incorrectHardness: 6.5-7 on Mohs scale. Color: Translucent orange to reddish-brown. Luster: Waxy to vitreous. Crystal Structure: Trigonal (cryptocrystalline). Cleavage: None (conchoidal fracture). Specific Gravity: 2.58-2.64.
- Hardness
- 6
- Color
- Translucent orange to reddish-brown
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 on Mohs scale. Color: Translucent orange to reddish-brown. Luster: Waxy to vitreous. Crystal Structure: Trigonal (cryptocrystalline). Cleavage: None (conchoidal fracture). Specific Gravity: 2.58-2.64.
Formation & geological history
Formed in low-temperature silica-rich environments, typically in volcanic rocks, cavities (geodes), or sedimentary deposits where silica-rich fluids permeate through rock. The color is caused by iron oxide impurities.
Uses & applications
Primarily used in jewelry for cabochons and beads, ornamental carvings, and widely collected as tumbled stones or mineral specimens.
Geological facts
Carnelian has been used for over 4,500 years; Romans used it for signet rings because hot wax does not stick to it. It was also considered a stone of courage and high energy in ancient Egypt.
Field identification & locations
Identify by its translucent waxy appearance and orange-red hue. It is commonly found in India, Brazil, Uruguay, and various river beds worldwide where volcanic rock has weathered.
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Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
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Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
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Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
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Granite
Granite (Phaneritic intrusive igneous rock)
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