
sedimentary
Chert / Microcrystalline Quartz
Chert (SiO2)
AI-generated identification · may be incorrectHardness: 7 (Mohs scale); Color: Light tan, grey, or greenish hues; Luster: Dull to waxy; Crystal structure: Cryptocrystalline (microscopic quartz crystals); Cleavage: None, exhibits conchoidal (shell-like) fracture; Specific Gravity: 2.65.
- Hardness
- 7 (Mohs scale)
- Color
- Light tan, grey, or greenish hues
- Luster
- Dull to waxy
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Physical properties
Hardness: 7 (Mohs scale); Color: Light tan, grey, or greenish hues; Luster: Dull to waxy; Crystal structure: Cryptocrystalline (microscopic quartz crystals); Cleavage: None, exhibits conchoidal (shell-like) fracture; Specific Gravity: 2.65.
Formation & geological history
Formed as a chemical precipitate from silica-rich fluids or the accumulation of siliceous remains of marine organisms (like radiolaria or diatoms) in deep-ocean settings. This specimen appears to be a weathered river stone or glacial pebble.
Uses & applications
Historically used for stone tools and arrowheads due to its sharp edges; currently used for road base, landscaping, and as a low-cost lapidary material for tumbling.
Geological facts
Chert has been used by humans for millions of years to make fire and tools. It is so hard that it can scratch steel. Some varieties, like flint, are functionally the same but occur in chalk or limestone beds.
Field identification & locations
Identify in the field by its hardness (it will scratch glass), conchoidal fracture patterns (curved break surfaces), and smooth, waxy texture when freshly broken. Found globally in sedimentary basins and stream beds.
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