
sedimentary
Chert (vuggy/nodular)
Microcrystalline Quartz (SiO2)
Hardness: 7 (Mohs scale); Color: Cream, tan, white, and grayish; Luster: Waxy to dull (earthy in weathered areas); Crystal Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
- Hardness
- 7 (Mohs scale)
- Color
- Cream, tan, white, and grayish
- Luster
- Waxy to dull (earthy in weathered areas)
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Physical properties
Hardness: 7 (Mohs scale); Color: Cream, tan, white, and grayish; Luster: Waxy to dull (earthy in weathered areas); Crystal Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
Formation & geological history
Formed through the precipitation of silica-rich fluids in sedimentary rock cavities or by the replacement of calcium carbonate in limestone. These specimens common date from the Paleozoic to Mesozoic eras.
Uses & applications
Used historically for tool-making (arrowheads, scrapers) due to sharp edges; currently used for decorative stone, road ballast, and as a collector specimen.
Geological facts
This specimen contains a vug (cavity) often referred to as a 'rattle stone' if the inner nodule is loose. Chert is extremely chemically stable and can survive millions of years of weathering.
Field identification & locations
Identify in the field by its hardness (it should scratch glass), waxy texture when freshly broken, and conchoidal (shell-like) fracture. Commonly found in riverbeds and eroded limestone outcrops.
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