
mineral
Chalcedony (Agate Pebble)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 on Mohs scale. Color: Greyish-blue interior with a rusty brown iron-stained exterior. Luster: Waxy to vitreous. Crystal Structure: Trigonally microcrystalline. Cleavage: None. Fracture: Conchoidal.
- Hardness
- 6
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 on Mohs scale. Color: Greyish-blue interior with a rusty brown iron-stained exterior. Luster: Waxy to vitreous. Crystal Structure: Trigonally microcrystalline. Cleavage: None. Fracture: Conchoidal.
Formation & geological history
Formed through the deposition of silica from groundwater in cavities of volcanic or sedimentary rocks. The weathered exterior suggests it was transported by water (alluvial) or exposed to prolonged oxidation.
Uses & applications
Used primarily in lapidary work for cabochons, beads, and carvings. Also used in industrial applications requiring high hardness and chemical resistance, such as mortars and pestles.
Geological facts
Chalcedony is a cryptocrystalline form of silica. This specific specimen shows a classic 'nodule' structure where the weathered outer rind protects the translucent interior. The blue-grey tint is common in varieties often called 'Blue Lace' or 'Cloud' chalcedony.
Field identification & locations
Identify in the field by its waxy luster, conchoidal (shell-like) fracture, and inability to be scratched by a steel knife. It is often found in riverbeds or areas with ancient volcanic activity.
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