
mineral
Banded Agate
Cryptocrystalline Quartz (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 on Mohs scale; Color: Multi-colored bands (brown, white, tan); Luster: Waxy to vitreous; Crystal structure: Trigonal/Microcrystalline; Cleavage: None; Specific Gravity: 2.58-2.64.
- Hardness
- 6
- Color
- Multi-colored bands (brown, white, tan)
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Multi-colored bands (brown, white, tan); Luster: Waxy to vitreous; Crystal structure: Trigonal/Microcrystalline; Cleavage: None; Specific Gravity: 2.58-2.64.
Formation & geological history
Formed in cavities within volcanic or sedimentary rocks where silica-rich groundwater deposits layers of quartz and chalcedony over time. Often found in ancient lava flows.
Uses & applications
Commonly used in lapidary work, jewelry making (cabochons), interior decor, and as healing stones in metaphysical practices.
Geological facts
The distinct banding in agates is caused by variations in the minerals present during different periods of deposition. It is the state gemstone of several US states including Minnesota.
Field identification & locations
Identified by its translucent properties when held to light and its characteristic parallel banding layers. Often found in riverbeds or near ancient volcanic sites globally.
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Epidote
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