
mineral
Dyed Blue Agate
Silicon Dioxide (SiO2) with artificial pigment
AI-generated identification · may be incorrectHardness: 6.5-7 on Mohs scale; Color: Intense neon/vivid blue with banding; Luster: Vitreous to waxy; Crystal structure: Trigonal/Microcrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.64
- Hardness
- 6
- Color
- Intense neon/vivid blue with banding
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Intense neon/vivid blue with banding; Luster: Vitreous to waxy; Crystal structure: Trigonal/Microcrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.64
Formation & geological history
Formed as chalcedony through the deposition of silica from groundwater in the cavities of igneous rocks. The intense blue color is achieved post-extraction by soaking the porous stone in ferric salts followed by a chromium or potassium ferrocyanide solution.
Uses & applications
Primarily used for decorative purposes, jewelry (pendants, beads), tumbled stones for collectors, and New Age healing practices.
Geological facts
Natural blue agate (Blue Lace Agate) is typically very pale lavender-blue. Any agate with this level of 'electric' blue saturation is almost certainly artificially dyed, a practice that dates back to the Roman Empire.
Field identification & locations
Identify by looking for concentrations of pigment in the tiny fractures or cracks of the stone. Natural blue minerals rarely show this specific shade of neon blue. Common sources of the base agate include Brazil and Uruguay.
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