Rock Identifier
Banded Agate (River Pebble) (Silicon Dioxide with impurities (SiO2)) — sedimentary
sedimentary

Banded Agate (River Pebble)

Silicon Dioxide with impurities (SiO2)

Hardness: 6.5-7 (Mohs scale); Color: Tan, brown, and cream concentric bands; Luster: Waxy to dull; Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.64.

Hardness
6
Color
Tan, brown, and cream concentric bands
Luster
Waxy to dull
Identified More sedimentary
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Physical properties

Hardness: 6.5-7 (Mohs scale); Color: Tan, brown, and cream concentric bands; Luster: Waxy to dull; Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.64.

Formation & geological history

Formed as secondary deposits in volcanic rock cavities or sedimentary geodes through the deposition of silica-rich groundwater. This specimen shows significant river-wear or tumble-smoothing. Geological age varies from 20 million to over 1 billion years depending on location.

Uses & applications

Polishing for lapidary use, ornamental stones, metaphysical collecting, and jewelry making.

Geological facts

Agate bands are formed by the periodic precipitating of silica from aqueous solution. Each layer represents a different pulse of mineral-rich water entering a void in the earth.

Field identification & locations

Identify by looking for distinct concentric banding patterns and a translucency when held to light. Commonly found in riverbeds, glacial tills, and volcanic regions like the Lake Superior area or Brazil.