
mineral
Blue Banded Agate
Chalcedony (Silicon Dioxide, SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 on Mohs scale. Color: Bright blue, white, and translucent bands. Luster: Waxy to vitreous. Crystal Structure: Trigonal (microcrystalline/cryptocrystalline). Cleavage: None. Specific Gravity: 2.58-2.64.
- Hardness
- 6
- Color
- Bright blue, white, and translucent bands
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 on Mohs scale. Color: Bright blue, white, and translucent bands. Luster: Waxy to vitreous. Crystal Structure: Trigonal (microcrystalline/cryptocrystalline). Cleavage: None. Specific Gravity: 2.58-2.64.
Formation & geological history
Formed by the deposition of silica from groundwater in the cavities of igneous rocks, primarily volcanic lava. The blue color in this specific specimen is enhanced through artificial dyeing, a common practice for agates.
Uses & applications
Used extensively in jewelry making for pendants and beads, decorative carvings, and as a healing stone in metaphysical practices. Industrial uses include mortars and pestles.
Geological facts
Agate was named by Theophrastus, a Greek philosopher, who discovered the stone along the shore line of the river Achates in present-day Sicily. Intense blue banding like this is almost always the result of staining porous chalcedony with iron salts.
Field identification & locations
Identify in the field by its distinct concentric banding and waxy appearance. Commonly found in Brazil, Uruguay, and India. Collectors look for unique patterns and transluency.
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