
mineral
Blue Agate (Dyed)
Silicon Dioxide (SiO2) - Microcrystalline Quartz
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs); Color: Naturally gray/white but dyed vibrant blue; Luster: Waxy to vitreous; Crystal Structure: Hexagonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.6 - 2.64.
- Hardness
- 6
- Color
- Naturally gray/white but dyed vibrant blue
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 (Mohs); Color: Naturally gray/white but dyed vibrant blue; Luster: Waxy to vitreous; Crystal Structure: Hexagonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.6 - 2.64.
Formation & geological history
Formed as secondary deposits in hollow cavities (geodes) of volcanic rocks (igneous) through the deposition of silica-rich groundwater. Agate formation takes millions of years throughout various geological eras.
Uses & applications
Primarily used for decorative purposes, lapidary arts, jewelry (cabochons), bookends, and 'tumbled stones' for collectors or metaphysical use.
Geological facts
Natural agate rarely occurs in this saturated shade of neon blue. Most blue agates on the market, like this specimen, are dyed using inorganic salts to enhance the aesthetic appeal and highlight the internal banding patterns.
Field identification & locations
Identify in the field by its waxy luster and translucency when held to light. To check for dye, look for concentrated pockets of pigment in cracks. Found globally in Brazil, Uruguay, and the USA (notably Lake Superior region).
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Epidote
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Granite
Granite (Phaneritic intrusive igneous rock)
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