
sedimentary
Chert (Likely Jasper)
Microcrystalline Quartz (SiO2)
AI-generated identification · may be incorrectHardness: 7 Mohs scale; Color: Honey-yellow, orange-brown, and white; Luster: Waxy to vitreous; Crystal Structure: Trigonal (Microcrystalline); Cleavage: None (Conchoidal fracture); Specific Gravity: 2.65
- Hardness
- 7 Mohs scale
- Color
- Honey-yellow, orange-brown, and white
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 7 Mohs scale; Color: Honey-yellow, orange-brown, and white; Luster: Waxy to vitreous; Crystal Structure: Trigonal (Microcrystalline); Cleavage: None (Conchoidal fracture); Specific Gravity: 2.65
Formation & geological history
Formed via the accumulation of silica-rich microfossils on the seafloor or through the replacement of limestone by silica-saturated groundwater. This specimen displays the typical conchoidal fractures of cryptocrystalline silica.
Uses & applications
Historically used for making stone tools (arrowheads). Modern uses include lapidary work, jewelry (tumbled stones), and as a decorative landscaping rock.
Geological facts
Chert and its varieties like Jasper and Flint were among the first resources used by early humans for tools because of how they shatter into extremely sharp edges.
Field identification & locations
Identified in the field by its waxy luster, hardness (it will scratch glass), and smooth, shell-like (conchoidal) fracture surfaces. Commonly found in sedimentary rock layers or as nodules in limestone.
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