
mineral
Carnelian Agate
Silicon Dioxide (SiO2) - variety of Chalcedony
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs), Color: Orange-red to brownish-red, Luster: Waxy to vitreous, Crystal Structure: Trigonal (microcrystalline/cryptocrystalline), Cleavage: None/Conchoidal fracture, Specific Gravity: 2.58-2.64
- Hardness
- 6
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Physical properties
Hardness: 6.5-7 (Mohs), Color: Orange-red to brownish-red, Luster: Waxy to vitreous, Crystal Structure: Trigonal (microcrystalline/cryptocrystalline), Cleavage: None/Conchoidal fracture, Specific Gravity: 2.58-2.64
Formation & geological history
Formed through the deposition of silica in gas cavities of volcanic rocks. The red-orange hue comes from iron oxide (hematite) impurities dispersed within the silica structure.
Uses & applications
Used primarily in lapidary arts, jewelry making (cabochons, beads), decorative carvings, and as a popular collector's tumbled stone.
Geological facts
Carnelian was used widely in the ancient world for cylinder seals and signet rings because hot wax does not stick to it. It has been mined since the Neolithic period.
Field identification & locations
Identify in the field by its translucency and waxy luster compared to jasper; look for it in volcanic riverbeds or coastal gravels in places like Brazil, India, or the Pacific Northwest, USA.
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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