
sedimentary
Banded Chert Pebble
Silicon Dioxide (SiO2) - Microcrystalline Quartz
Hardness: 6.5-7 on Mohs scale; Color: Dark grey to black with brownish-tan quartz/chalcedony veins and banding; Luster: Waxy to sub-vitreous; Structure: Cryptocrystalline/microcrystalline; Cleavage: None, exhibits conchoidal fracture.
- Hardness
- 6
- Luster
- Waxy to sub-vitreous
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: Dark grey to black with brownish-tan quartz/chalcedony veins and banding; Luster: Waxy to sub-vitreous; Structure: Cryptocrystalline/microcrystalline; Cleavage: None, exhibits conchoidal fracture.
Formation & geological history
Formed through the accumulation of silica-rich biogenic sediments (such as radiolarian shells or diatoms) or precipitation from hydrothermal fluids. Stream-tumbled and smoothed in riverbed environments over geological timescales.
Uses & applications
Historically used for stone tools and fire-starting due to its hardness and sharp conchoidal fracturing. Modern usage includes decorative landscaping, aquariums, lapidary polishing, and tumbled rock collections.
Geological facts
Chert is extremely durable and chemically resistant. Black varieties are often called basanite or touchstone, historically used by goldsmiths to test the purity of precious metals by observing the streak color.
Field identification & locations
Identified by its high hardness (scratches glass), waxy luster, smooth rounded pebble shape, and distinct yellowish/tan veining running through a dark matrix. Commonly found along riverbeds, gravel bars, and beaches.
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