Rock Identifier
Banded Chert (Agate) (Silicon Dioxide (SiO2)) — sedimentary
sedimentary

Banded Chert (Agate)

Silicon Dioxide (SiO2)

Hardness: 7 Mohs; Color: Brown, tan, and white banding; Luster: Waxy to vitreous; Crystal Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.6

Hardness
7 Mohs
Color
Brown, tan, and white banding
Luster
Waxy to vitreous
Identified More sedimentary

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Physical properties

Hardness: 7 Mohs; Color: Brown, tan, and white banding; Luster: Waxy to vitreous; Crystal Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.6

Formation & geological history

Formed as a microcrystalline sedimentary rock from the precipitation of silica in groundwater or from the accumulation of silica-rich microfossils. These specimens often originate in marine environments or volcanic cavities.

Uses & applications

Used primarily for lapidary work, jewelry (beads and cabochons), and as landscaping stones. Historically used for making sharp tools like arrowheads due to its conchoidal fracture.

Geological facts

Banded chert is often transitionally related to agate. The distinct layers reflect changes in the chemistry of the silica-rich fluids during the accumulation or deposition process.

Field identification & locations

Identify in the field by its hardness (will scratch glass), waxy appearance, and smooth, rounded surface when tumbled by water. Commonly found in riverbeds, glacial tills, and coastal beaches.