
mineral
Banded Agate (specifically sardonyx or carnelian agate variety)
Silicon Dioxide (SiO2) - Cryptocrystalline Quartz
Hardness: 6.5-7 (Mohs scale); Color: Translucent white to tan with orange/red-brown concentric bands; Luster: Waxy to vitreous; Crystal structure: Trigonal/Hexagonal (microscopic); Cleavage: None (conchoidal fracture); Specific gravity: 2.58-2.64
- Hardness
- 6
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Translucent white to tan with orange/red-brown concentric bands; Luster: Waxy to vitreous; Crystal structure: Trigonal/Hexagonal (microscopic); Cleavage: None (conchoidal fracture); Specific gravity: 2.58-2.64
Formation & geological history
Formed primarily in volcanic environments where silica-rich groundwater fills cavities (vesicles) in lava flows. Layering occurs through rhythmic deposition of silica over thousands of years. Age varies by tectonic region, often ranging from 10 to 100 million years old.
Uses & applications
Used widely in lapidary arts for jewelry, beads, and carvings. Historically used for making signet rings and cameos. In industry, it is used to make burnishers or mortars and pestles due to its hardness.
Geological facts
Agate is named after the Achates River in Sicily where it was first discovered. The 'eye' patterns sometimes found in these stones were historically believed to ward off the 'evil eye'. It is the birthstone for September and the 12th wedding anniversary stone.
Field identification & locations
Identify in the field by its distinct translucent concentric bands and waxy texture when wet. Commonly found in riverbeds, gravel pits, and coastal areas near ancient volcanic activity (e.g., Lake Superior region, Brazil, India). To collect, look for stones with a 'potato-skin' texture on the outside that reveal banding when chipped or sliced.
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