
mineral
Chalcedony (Agate/Chert)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale); Color: Blue-grey to tan/brown; Luster: Waxy to vitreous; Crystal structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.58-2.64
- Hardness
- 6
- Color
- Blue-grey to tan/brown
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Blue-grey to tan/brown; Luster: Waxy to vitreous; Crystal structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.58-2.64
Formation & geological history
Formed as a chemical precipitate from silica-rich hydrothermal fluids or groundwater, often filling cavities (vesicles) in volcanic rocks or within sedimentary limestone nodules.
Uses & applications
Commonly used in jewelry for cabs and beads, as ornamental stone carvings, and historically for stone tools due to its conchoidal fracture which creates sharp edges.
Geological facts
Chalcedony is a cryptocrystalline form of silica, meaning its crystals are so small they can only be seen under high magnification. It is the base mineral for agate, jasper, and onyx.
Field identification & locations
Identify by its waxy luster, translucency, and shell-like (conchoidal) fracture surfaces. Commonly found in gravel beds, desert pavements, and volcanic regions worldwide.
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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
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
Septarian Pebble
Septarian nodule / Concretion
sedimentary