
sedimentary
Chert (Jasper/Chalcedony variety)
Microcrystalline Quartz (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 on Mohs scale; Color: honey-yellow, orange-brown, and tan; Luster: waxy to vitreous; Crystal structure: Trigonal (microcrystalline); Cleavage: none, exhibits conchoidal fracture; Specific gravity: 2.6-2.65
- Hardness
- 6
- Color
- honey-yellow, orange-brown, and tan
- Luster
- waxy to vitreous
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Physical properties
Hardness: 6.5-7 on Mohs scale; Color: honey-yellow, orange-brown, and tan; Luster: waxy to vitreous; Crystal structure: Trigonal (microcrystalline); Cleavage: none, exhibits conchoidal fracture; Specific gravity: 2.6-2.65
Formation & geological history
Formed through the accumulation of silica-rich fluids in sedimentary basins or by the replacement of limestone. This specimen likely formed during the Cenozoic or Mesozoic eras through chemical precipitation.
Uses & applications
Historically used for stone tools (knapping); currently used for lapidary work, jewelry (cabochons), and as a decorative landscaping rock.
Geological facts
Because of its high hardness and conchoidal fracture, this material was one of the most important resources for prehistoric humans to create sharp-edged arrowheads and knives.
Field identification & locations
Identify by its 'waxy' appearance, hardness (it will scratch glass), and the shell-like (conchoidal) curves where it has chipped. Commonly found in riverbeds, desert pavements, and limestone outcrops.
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