
sedimentary
Chert (variously known as Flint or Jasper)
Microcrystalline or Cryptocrystalline Quartz (SiO2)
Hardness: 7 on Mohs scale. Color: Tan, beige, light brown, white. Luster: Dull to waxy. Crystal Structure: Trigonal (microscopic). Cleavage: None (conchoidal fracture). Specific gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Color
- Tan, beige, light brown, white
- Luster
- Dull to waxy
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Physical properties
Hardness: 7 on Mohs scale. Color: Tan, beige, light brown, white. Luster: Dull to waxy. Crystal Structure: Trigonal (microscopic). Cleavage: None (conchoidal fracture). Specific gravity: 2.65.
Formation & geological history
Formed by the precipitation of silica from seawater or groundwater. Commonly occurs as nodules in limestone or chalk beds. Often associated with Precambrian to Holocene geological ages.
Uses & applications
Historically used for stone tools and weapons due to sharp fracture edges. Today used in construction aggregate, road surfacing, and as a decorative stone in landscaping.
Geological facts
Chert was one of the most important minerals for early humans because its conchoidal fracture creates edges sharper than a steel scalpel. Native Americans used it extensively for arrowheads.
Field identification & locations
Identify in the field by its hardness (it scrapes steel and glass) and the characteristic curved, shell-like (conchoidal) fracture pattern when broken. It is extremely common globally in sedimentary outcrops.
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