
mineral
Carnelian Agate
Silicon dioxide (SiO2) - Chalcedony variety
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale); Color: Orange, reddish-brown, semi-translucent with banding; Luster: Waxy to vitreous; Crystal structure: Hexagonal (trigonal) cryptocrystalline; Cleavage: None; Specific gravity: 2.58-2.64
- Hardness
- 6
- Color
- Orange, reddish-brown, semi-translucent with banding
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Orange, reddish-brown, semi-translucent with banding; Luster: Waxy to vitreous; Crystal structure: Hexagonal (trigonal) 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, particularly volcanic lavas. The reddish-orange tint is caused by iron oxide impurities.
Uses & applications
Primarily used in jewelry (beads, cabochons), ornamental carvings, and as a semi-precious collector gemstone or healing stone.
Geological facts
In ancient Egypt, Carnelian was often placed on mummies to assist in the soul's journey into the afterlife. It is one of the oldest gemstones used for seals and signet rings.
Field identification & locations
Identify by its waxy luster, translucency, and warm orange-red color. It is common in river gravels and volcanic regions. Look for conchoidal fractures when broken.
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Other mineral specimens
Gneiss or Schist
Gneiss or Mica Schist with Garnet
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