
sedimentary
Chert (Arrowhead Fragment)
Microcrystalline Quartz (SiO2)
Hardness: 7 (Mohs scale); Color: Gray, brown, and translucent tan; Luster: Waxy to vitreous; Crystal Structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 (Mohs scale)
- Color
- Gray, brown, and translucent tan
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 7 (Mohs scale); Color: Gray, brown, and translucent tan; Luster: Waxy to vitreous; Crystal Structure: Trigonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed through the accumulation of silica-rich organic remains or chemical precipitation in sedimentary environments. Specimen shows evidence of anthropogenic knapping (flake scars) indicative of stone tool manufacturing.
Uses & applications
Historically used for making stone tools (arrowheads, scrapers, knives) due to its sharp conchoidal fracture. Currently valued as an archaeological artifact and for lapidary use.
Geological facts
Chert was one of the most important minerals for early humans. This specimen appears to be a bifacially worked fragment or a large percussion flake from a lithic reduction process.
Field identification & locations
Identify in the field by its waxy texture, inability to be scratched by steel, and sharp, shell-like (conchoidal) fracture points. Commonly found in limestone and chalk formations.
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