
sedimentary
Chert / Jasper
Microcrystalline Quartz (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale); Color: Variegated brown, tan, and reddish-orange; Luster: Waxy to vitreous (especially when wet); Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.6-2.7
- Hardness
- 6
- Color
- Variegated brown, tan, and reddish-orange
- Luster
- Waxy to vitreous (especially when wet)
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Variegated brown, tan, and reddish-orange; Luster: Waxy to vitreous (especially when wet); Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.6-2.7
Formation & geological history
Formed through the accumulation of silica-rich microfossils or chemical precipitation from hydrothermal fluids in sedimentary environments. Common in marine or lake deposits from various geological eras, including Paleozoic to Cenozoic.
Uses & applications
Historically used for stone tools (knapping); modernly used for lapidary work, decorative landscaping, and as river rock. Polished specimens are used in jewelry.
Geological facts
This specimen appears to be a 'river rock' or 'glacial cobble' that has been naturally smoothed by water. The reddish tints indicate iron oxide inclusions within the silica matrix.
Field identification & locations
Identify in the field by its hardness (it should scratch glass), waxy appearance, and conchoidal (shell-like) fracture edges. These are ubiquitous in riverbeds and glacial tills across North America and Europe.
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