
mineral
Banded Agate
Agate (Silicon Dioxide, SiO2)
Hardness: 6.5-7 Mohs; Color: Varied bands of grey, blue-grey, and white; Luster: Vitreous to waxy; Crystal structure: Trigonal (cryptocrystalline); Specific gravity: 2.58-2.64.
- Hardness
- 6
- Color
- Varied bands of grey, blue-grey, and white
- Luster
- Vitreous to waxy
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Physical properties
Hardness: 6.5-7 Mohs; Color: Varied bands of grey, blue-grey, and white; Luster: Vitreous to waxy; Crystal structure: Trigonal (cryptocrystalline); Specific gravity: 2.58-2.64.
Formation & geological history
Formed in cavities of volcanic rocks (lavas) or certain metamorphic rocks through the deposition of silica from groundwater. The bands are formed by successive layers of silica being deposited over millennia.
Uses & applications
Used widely in lapidary arts for jewelry, decorative ornaments, bookends, and collection. Historically used for making hardstone carvings and precision instrument bearings.
Geological facts
The name 'Agate' comes from the Achates River in Sicily, where agates were first discovered. Unlike many minerals, the banding in agate is caused by rhythmic crystallization.
Field identification & locations
Identify in the field by its characteristic concentric banding, waxy luster when broken, and extreme hardness (it will scratch glass). Commonly found in river beds, beaches, and volcanic regions.
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