
sedimentary
Chert (specifically Tan/Gray Chert)
Microcrystalline quartz (SiO2)
Hardness: 7 (Mohs); Color: Tan, brownish-gray; Luster: Waxy to dull; Crystal structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.65
- Hardness
- 7 (Mohs)
- Color
- Tan, brownish-gray
- Luster
- Waxy to dull
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Physical properties
Hardness: 7 (Mohs); Color: Tan, brownish-gray; Luster: Waxy to dull; Crystal structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.65
Formation & geological history
Formed through the accumulation of siliceous remains of organisms (like diatoms or radiolarians) or by the precipitation of silica from groundwater within sedimentary rock layers, often limestone.
Uses & applications
Historically used for stone tools (knapping) due to its sharp edges; used today in road construction aggregate and sometimes as a minor gemstone when colorful (Jasper).
Geological facts
Chert has a conchoidal fracture, which means it breaks like glass. This property made it the primary material for prehistoric arrowheads and scrapers.
Field identification & locations
Identify in the field by its hardness (it can scratch glass), waxy appearance, and shell-like fracture patterns. Common in limestone outcrops and riverbeds.
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