
sedimentary
Chert (Jasper variety)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale); Color: Reddish-brown, tan, and yellow due to iron oxide inclusions; Luster: Dull to waxy; Crystal Structure: Cryptocrystalline (microscopic quartz); Cleavage: None (conchoidal fracture); Specific Gravity: 2.6-2.7
- Hardness
- 6
- Color
- Reddish-brown, tan, and yellow due to iron oxide inclusions
- Luster
- Dull to waxy
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Reddish-brown, tan, and yellow due to iron oxide inclusions; Luster: Dull to waxy; Crystal Structure: Cryptocrystalline (microscopic quartz); Cleavage: None (conchoidal fracture); Specific Gravity: 2.6-2.7
Formation & geological history
Formed through the accumulation of silica-rich organic remains (like diatoms) or chemical precipitation from hydrothermal fluids in sedimentary environments. Common in ancient limestone or dolomite beds.
Uses & applications
Historically used for stone tools (arrowheads/scrapers) due to its sharp conchoidal fracture. Today used for lapidary work, landscaping, and as a collector specimen.
Geological facts
Jasper is an opaque variety of chalcedony. The reddish hues in this specimen are likely caused by impurities of hematite (iron oxide). It was one of the primary materials used by Paleolithic humans for tool-making.
Field identification & locations
Identify in the field by its hardness (cannot be scratched by a steel knife) and its conchoidal (shell-like) fracture edges. Commonly found in riverbeds or within sedimentary rock outcrops.
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