Rock Identifier
Banded Agate (Silicon Dioxide (SiO2) - Chalcedony variety) — mineral
mineral

Banded Agate

Silicon Dioxide (SiO2) - Chalcedony variety

Hardness: 6.5-7 (Mohs scale). Color: White, gray, and blue-gray bands. Luster: Waxy to vitreous. Crystal structure: Cryptocrystalline (Trigonal). Cleavage: None (Conchoidal fracture). Specific Gravity: 2.60-2.65.

Hardness
6
Color
White, gray, and blue-gray bands
Luster
Waxy to vitreous
Identified More mineral

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Physical properties

Hardness: 6.5-7 (Mohs scale). Color: White, gray, and blue-gray bands. Luster: Waxy to vitreous. Crystal structure: Cryptocrystalline (Trigonal). Cleavage: None (Conchoidal fracture). Specific Gravity: 2.60-2.65.

Formation & geological history

Formed primarily in volcanic and metamorphic environments. Silica-rich groundwater fills cavities (vugs) in host rock, depositing layers of microcrystalline quartz over time. Most specimens occur in ancient basaltic lava flows.

Uses & applications

Used widely in lapidary arts for jewelry, beads, and polished palm stones. Also used in industry for mortar and pestles due to its hardness, and for precision pendulums and balances.

Geological facts

Agate was named by Theophrastus, a Greek philosopher, who discovered the stone along the shore of the Achates River in Sicily. No two agates are exactly alike due to the unique layering process during formation.

Field identification & locations

Identify in the field by its waxy appearance, translucency at edges, and characteristic concentric or parallel banding. Commonly found in riverbeds, lakeshores (like Lake Superior), and volcanic regions. Collectors look for unbroken bands and high translucency.