
mineral
Banded Agate
Silicon Dioxide (SiO2) - Variety Agate
AI-generated identification · may be incorrectHardness: 6.5-7 Mohs; Color: Gray, white, and yellow banding; Luster: Waxy to vitreous; Crystal Structure: Hexagonal (cryptocrystalline); Cleavage: None; Fracture: Conchoidal.
- Hardness
- 6
- Color
- Gray, white, and yellow banding
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 Mohs; Color: Gray, white, and yellow banding; Luster: Waxy to vitreous; Crystal Structure: Hexagonal (cryptocrystalline); Cleavage: None; Fracture: Conchoidal.
Formation & geological history
Formed in volcanic or metamorphic rocks, typically filling cavities or veins. These bands occur through the rhythmic deposition of silica from groundwater over long periods.
Uses & applications
Commonly used in jewelry (cabochons, beads), decorative objects, and historically for making mortars and pestles due to its hardness and resistance to chemicals.
Geological facts
Agate is named after the Achates River in Sicily where it was first discovered. The distinct banding is caused by variations in the mineral and impurity content during the slow growth process.
Field identification & locations
Identify in the field by its waxy luster, conchoidal fracture, and characteristic banding. Often found as nodules in gravel beds or volcanic regions like Brazil, India, and the United States (Lake Superior region).
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Septarian Pebble
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