
sedimentary
Green Chert (Jasper)
Silicon Dioxide (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale); Color: Olive green to moss green; Luster: Waxy to vitreous; Crystal structure: Cryptocrystalline (Microcrystalline); Cleavage: None (has conchoidal fracture); Specific gravity: 2.58-2.91
- Hardness
- 6
- Color
- Olive green to moss green
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 6.5-7 (Mohs scale); Color: Olive green to moss green; Luster: Waxy to vitreous; Crystal structure: Cryptocrystalline (Microcrystalline); Cleavage: None (has conchoidal fracture); Specific gravity: 2.58-2.91
Formation & geological history
Formed through the accumulation of silica-rich microfossils (like radiolarians or diatoms) or chemical precipitation from hydrothermal fluids in marine environments. This specimen shows a waxy luster and conchoidal fractures typical of chert/jasper varieties.
Uses & applications
Historically used for stone tools (knapping) due to its sharp edges; modernly used as a lapidary material, in jewelry, and for ornamental stone collection.
Geological facts
Green chert is sometimes called 'Green Jasper' or 'Prase'. Because of its extreme hardness and the way it breaks into razor-sharp edges, it was a primary material for prehistoric arrowheads and scrapers.
Field identification & locations
Identify in the field by its waxy appearance, sharp curved (conchoidal) edges when broken, and it should be hard enough to scratch glass. Commonly found in stream beds, gravel deposits, and sedimentary limestone formations globally.
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