
mineral
Agate
Agate (Silicon Dioxide - SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 on Mohs scale; Color: Multi-colored (this specimen shows translucent honey, orange, and white banding); Luster: Waxy to vitreous; Crystal Structure: Cryptocrystalline (Trigonal/Monoclinic); Cleavage: None; Specific Gravity: 2.58-2.64.
- Hardness
- 6
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Multi-colored (this specimen shows translucent honey, orange, and white banding); Luster: Waxy to vitreous; Crystal Structure: Cryptocrystalline (Trigonal/Monoclinic); Cleavage: None; Specific Gravity: 2.58-2.64.
Formation & geological history
Formed in microcrystalline layers within the cavities of volcanic rocks (especially basalt) or some sedimentary rocks, where silica-rich groundwater gradually precipitates. Ages vary from Cenozoic to Precambrian depending on the host rock.
Uses & applications
Commonly used in jewelry (cabochons), lapidary art, decorative ornaments, and industrial applications such as precision mortar and pestles due to its hardness and chemical resistance.
Geological facts
Agate is a variety of chalcedony. The name comes from the Achates River in Sicily, where it was first discovered in ancient times. No two agates are exactly alike due to the unique rhythm of mineral deposition.
Field identification & locations
Identify in the field by its characteristic translucency when held to light, waxy texture, conchoidal fracture, and concentric 'iris' or 'landscape' banding. Frequently found in riverbeds, lake shores (like Lake Superior), and volcanic regions.
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