
mineral
Chalcedony / Agate
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 on Mohs scale; Color: Translucent white, grey, or yellowish with brown inclusions; Luster: Waxy to vitreous; Crystal Structure: Trigonal (cryptocrystalline); Cleavage: None; Specific Gravity: 2.58-2.64
- Hardness
- 6
- Color
- Translucent white, grey, or yellowish with brown inclusions
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Translucent white, grey, or yellowish with brown inclusions; Luster: Waxy to vitreous; Crystal Structure: Trigonal (cryptocrystalline); Cleavage: None; Specific Gravity: 2.58-2.64
Formation & geological history
Formed as a chemical precipitate from silica-rich hydrothermal fluids or groundwater, often filling cavities in volcanic or sedimentary rocks over thousands of years.
Uses & applications
Used primarily in lapidary work for jewelry, cabochons, and decorative ornamental items. Historically used for making stone tools due to its conchoidal fracture.
Geological facts
The name 'Chalcedony' comes from the ancient Greek town of Chalkedon. It is a microcrystalline form of quartz where the crystals are too small to be seen without high magnification.
Field identification & locations
Identify in the field by its translucency, waxy luster, and lack of visible crystal faces. Can be found globally in riverbeds, desert pavements, and volcanic outcrops.
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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