
sedimentary
Chert Concretion
Silicon dioxide (SiO2)
Hardness: 6.5-7 Mohs; Color: Tan, brown, or gray; Luster: Waxy to dull; Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.5-2.8
- Hardness
- 6
- Color
- Tan, brown, or gray
- Luster
- Waxy to dull
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Physical properties
Hardness: 6.5-7 Mohs; Color: Tan, brown, or gray; Luster: Waxy to dull; Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific gravity: 2.5-2.8
Formation & geological history
Formed through the precipitation of silica within porous sedimentary layers, typically limestone or chalk. These often grow around a nucleus like a fossil or a cavity during diagenesis millions of years ago.
Uses & applications
Historically used for making stone tools; today used in construction decorative stones and for geological education.
Geological facts
Chert is so hard it can scratch glass. It was one of the primary materials used by prehistoric humans to create arrowheads and scrapers due to its sharp edges when broken.
Field identification & locations
Identify in the field by its unusual, often bulbous or lumpy shape and high hardness compared to surrounding limestone. Frequently found in riverbeds or eroded limestone cliffs.
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Cone-in-cone structure (Secondary Sedimentary Structure)
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Chert Breccia
Brecciated Chert (Microcrystalline Silica)
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