
mineral
Carnelian Agate
Silicon dioxide (SiO2) with iron oxide impurities
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs); Color: Waxy reddish-brown to orange; Luster: Vitreous to waxy; Crystal Structure: Hexagonal (trigonal) microcrystalline silica; Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.64
- Hardness
- 6
- Color
- Waxy reddish-brown to orange
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5-7 (Mohs); Color: Waxy reddish-brown to orange; Luster: Vitreous to waxy; Crystal Structure: Hexagonal (trigonal) microcrystalline silica; Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.64
Formation & geological history
Formed in volcanic and sedimentary rocks as groundwater rich in silica precipitates in cavities. The distinctive orange-red color is caused by iron oxide (hematite) inclusions.
Uses & applications
Primarily used in jewelry for beads, cabochons, and intaglios. Also highly valued in spiritual and decorative lapidary arts.
Geological facts
Carnelian was used by ancient Egyptians for amulets and by Romans for signet rings because hot wax does not stick to it. It has been a prized gemstone for over 4,500 years.
Field identification & locations
Identified by its waxy luster, translucency, and warm color range. Commonly found in Brazil, India, Uruguay, and Madagascar. Collectors look for uniform color and high translucency.
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Gneiss or Schist
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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
igneous
Granite
Granite (Phaneritic intrusive igneous rock)
igneous