
mineral
Banded Agate / Chalcedony
Silicon Dioxide (SiO2) with trace impurities
Hardness: 6.5-7 on Mohs scale. Color: Brown, tan, and white banding. Luster: Waxy to vitreous. Structure: Cryptocrystalline. Cleavage: None (conchoidal fracture). Specific Gravity: 2.58–2.64.
- Hardness
- 6
- Color
- Brown, tan, and white banding
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 on Mohs scale. Color: Brown, tan, and white banding. Luster: Waxy to vitreous. Structure: Cryptocrystalline. Cleavage: None (conchoidal fracture). Specific Gravity: 2.58–2.64.
Formation & geological history
Formed in cavities (vesicles) of volcanic rocks or sedimentary environments through the deposition of silica-rich groundwater. Agates occur in rocks ranging from Precambrian to Cenozoic age.
Uses & applications
Used primarily for jewelry (cabochons), lapidary art, collection, and precision instruments like pendulum pivots and mortars/pestles due to its hardness.
Geological facts
Agate is a variety of chalcedony distinguished by its distinctive banding. It was named by the Greek philosopher Theophrastus after the Achates River in Sicily where it was first discovered.
Field identification & locations
Identify in the field by its waxy luster, smooth conchoidal fracture, and characteristic concentric or parallel banding when viewed under light. Commonly found in gravel beds or volcanic regions.
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