
sedimentary
Chert (specifically Jasper)
Silicon dioxide (SiO2) with iron oxide inclusions
Hardness: 6.5-7 (Mohs); Color: Mottled green, reddish-brown, and grey; Luster: Dull to waxy; Structure: Microcrystalline/Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.91
- Hardness
- 6
- Color
- Mottled green, reddish-brown, and grey
- Luster
- Dull to waxy
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Physical properties
Hardness: 6.5-7 (Mohs); Color: Mottled green, reddish-brown, and grey; Luster: Dull to waxy; Structure: Microcrystalline/Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.58-2.91
Formation & geological history
Formed through the accumulation of silica-rich microfossils or chemical precipitation from hydrothermal fluids in sedimentary environments. Can be found in geological formations spanning billions of years, often in nodules or bedded deposits.
Uses & applications
Historically used for stone tools (knapping) due to its sharp edges; modernly used for lapidary work, jewelry (cabochons), and landscaping stones.
Geological facts
Jasper is an opaque variety of chalcedony. Its colors are caused by impurities; the reddish tones in this specimen are likely due to hematite (iron oxide). It was one of the first materials used by early humans for tools because of its predictable fracture patterns.
Field identification & locations
Identify in the field by its hardness (it will scratch glass), smooth waxy feel, and characteristic shell-like (conchoidal) fractures. Found globally, especially in riverbeds or marine sedimentary rock outcrops.
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