
mineral
Carnelian (Orange Agate/Chalcedony)
Silicon Dioxide (SiO2) - variety of Chalcedony
AI-generated identification · may be incorrectHardness: 6.5-7 on Mohs scale; Color: Orange to reddish-brown; Luster: Waxy to vitreous; Crystal Structure: Hexagonal (trigonal) microcrystalline; Cleavage: None; Specific Gravity: 2.58-2.64
- Hardness
- 6
- Color
- Orange to reddish-brown
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Orange to reddish-brown; Luster: Waxy to vitreous; Crystal Structure: Hexagonal (trigonal) microcrystalline; 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, particularly volcanic lavas. The orange color comes from iron oxide (hematite) impurities.
Uses & applications
Used primarily as a semi-precious gemstone in jewelry (beads, cabochons), carved seals, and as decorative pocket stones for collectors.
Geological facts
Carnelian was widely used in ancient Rome for signet rings and seals because hot wax does not stick to it. It has been used for jewelry since the Neolithic period.
Field identification & locations
Identify in the field by its waxy luster, conchoidal (shell-like) fracture, and translucent orange hue. Often found in riverbeds or on beaches in volcanic regions.
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Metamorphic
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Tumbled granite
Granite, a coarse-grained felsic intrusive igneous rock
igneous
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