
sedimentary
Chert (Green Chert or Jasper)
Silicon Dioxide (SiO2)
Hardness: 6.5-7 (Mohs); Color: Dark green with yellow/brown iron staining; Luster: Waxy to dull; Crystal structure: Microcrystalline/Cryptocrystalline; Cleavage: None (Conchoidal fracture)
- Hardness
- 6
- Color
- Dark green with yellow/brown iron staining
- Luster
- Waxy to dull
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Physical properties
Hardness: 6.5-7 (Mohs); Color: Dark green with yellow/brown iron staining; Luster: Waxy to dull; Crystal structure: Microcrystalline/Cryptocrystalline; Cleavage: None (Conchoidal fracture)
Formation & geological history
Formed as a chemical precipitate or by the replacement of carbonate rocks by silica-rich fluids. Often associated with ancient deep-sea deposits or volcanic hydrothermal activity.
Uses & applications
Historically used for making stone tools (arrowheads). Currently used as decorative landscaping stone, in lapidary work for cabochons, and as a collector's specimen.
Geological facts
Chert is so hard it can produce sparks when struck against steel. The green color is typically caused by the presence of chlorite or celadonite minerals within the silica matrix.
Field identification & locations
Identify in the field by its waxy texture and shell-like (conchoidal) fracture patterns. It cannot be scratched by a steel knife. Commonly found in riverbeds or as nodules in limestone.
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Cone-in-cone structure (Secondary Sedimentary Structure)
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Chert Breccia
Brecciated Chert (Microcrystalline Silica)
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Sandstone Grain
Clastic Sedimentary Rock Grain (SiO2 dominated)
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Shale or Slaty Mudstone
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Arenite (primarily SiO2)
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