
Mineral
Carnelian Agate
Silicon Dioxide (SiO2) - variety Carnelian (Chalcedony)
AI-generated identification · may be incorrectHardness: 6.5-7 on Mohs scale; Color: Translucent orange to reddish-brown; Luster: Vitreous to waxy; Crystal structure: Trigonal (microcrystalline/cryptocrystalline); Cleavage: None; Specific Gravity: 2.58–2.64
- Hardness
- 6
- Color
- Translucent orange to reddish-brown
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Translucent orange to reddish-brown; Luster: Vitreous to waxy; Crystal structure: Trigonal (microcrystalline/cryptocrystalline); Cleavage: None; Specific Gravity: 2.58–2.64
Formation & geological history
Formed through the deposition of silica from groundwater in the cavities of igneous rocks. The orange color is caused by iron oxide impurities. These specimens are often hundreds of millions of years old and are frequently found as river-worn nodules.
Uses & applications
Commonly used in lapidary work, cabochon jewelry, beads, and as decorative pocket stones or carvings.
Geological facts
Carnelian was widely used in ancient Rome and Egypt for signet rings and amulets because wax does not stick to its smooth surface. It is often heat-treated commercially to enhance the red/orange saturation.
Field identification & locations
Identify in the field by its translucency when held to light, waxy texture, and lack of visible crystal faces. Common in gravel pits, riverbeds, and beaches, particularly in the Pacific Northwest (USA), Brazil, and India.
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Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
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Granite, a coarse-grained felsic intrusive igneous rock
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Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Pegmatite with Tourmaline and Quartz
Igneous Pegmatite
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Granite
Granite (Phaneritic intrusive igneous rock)
igneous