
mineral
Blue Dyed Agate Geode Slice
Chalcedony (Silicon Dioxide, SiO2) with artificial cobalt/iron-based dye
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs); Color: Dyed vibrant blue (naturally gray/white); Luster: Vitreous to waxy; Structure: Trigonal crypto-crystalline; Cleavage: None; Specific Gravity: 2.58-2.64
- Hardness
- 6
- Color
- Dyed vibrant blue (naturally gray/white)
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5-7 (Mohs); Color: Dyed vibrant blue (naturally gray/white); Luster: Vitreous to waxy; Structure: Trigonal crypto-crystalline; Cleavage: None; Specific Gravity: 2.58-2.64
Formation & geological history
Formed in cavities of volcanic rocks or ancient lavas. Silica-rich groundwater percolates into bubbles (vesicles), depositing layers of chalcedony over thousands of years. This specific specimen has been chemically dyed.
Uses & applications
Decorative display, geophysics education, jewelry making, and metaphysical collecting. Sliced and polished to highlight internal banding.
Geological facts
While the banding and crystal center are natural, true blue agate is rare and usually a pale lavender-blue. This intense neon-blue is achieved by soaking the porous rock in chemical salts like potassium ferricyanide or ferrous sulfate.
Field identification & locations
Identified by concentric banding and a druzy quartz center. Look for unnaturally bright colors or dye concentrated in cracks to distinguish from natural blue lace agate. Common in Brazil and Uruguay.
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