
sedimentary
Chert (often called Jasper or Flint)
Microcrystalline Quartz (SiO2)
AI-generated identification · may be incorrectHardness: 6.5-7 (Mohs scale), Color: Red, brown, and gray variegation (impure), Luster: Waxy to vitreous, Crystal structure: Trigonal/Microcrystalline, Cleavage: None (conchoidal fracture), Specific gravity: 2.65
- Hardness
- 6
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Physical properties
Hardness: 6.5-7 (Mohs scale), Color: Red, brown, and gray variegation (impure), Luster: Waxy to vitreous, Crystal structure: Trigonal/Microcrystalline, Cleavage: None (conchoidal fracture), Specific gravity: 2.65
Formation & geological history
Formed through the accumulation of silica-rich organic remains or chemical precipitation in marine or freshwater environments. This specimen likely formed as a nodule in limestone or chalk during various geological eras (Paleozoic to Cenozoic).
Uses & applications
Historically used for stone tools (knapping). Currently used for lapidary work, jewelry (beads/cabochons), and as decorative landscaping stone.
Geological facts
Because it breaks with a conchoidal (shell-like) fracture, it produces very sharp edges. Early humans used this property to create spearheads and knives. It is also often used as the 'flint' in flint-and-steel fire starters.
Field identification & locations
Identify in the field by its waxy texture, smooth conchoidal fractures, and ability to scratch glass. Commonly found in riverbeds, glacial deposits, and as nodules in sedimentary rock layers across North America and Europe.
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