
sedimentary
Chert
Microcrystalline Quartz (SiO2)
Hardness: 7 on Mohs scale; Color: Light gray, white, tan, or brown; Luster: Waxy to vitreous; Crystal structure: Microcrystalline/cryptocrystalline quartz (chalcedony); Cleavage: None, exhibits conchoidal fracture; Specific gravity: 2.60 - 2.65
- Hardness
- 7 on Mohs scale
- Color
- Light gray, white, tan, or brown
- Luster
- Waxy to vitreous
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Physical properties
Hardness: 7 on Mohs scale; Color: Light gray, white, tan, or brown; Luster: Waxy to vitreous; Crystal structure: Microcrystalline/cryptocrystalline quartz (chalcedony); Cleavage: None, exhibits conchoidal fracture; Specific gravity: 2.60 - 2.65
Formation & geological history
Formed through the chemical precipitation of silica from aqueous solutions, often derived from the skeletal remains of marine microorganisms (like diatoms or radiolarians) accumulating in deep-marine environments or via the replacement of limestone.
Uses & applications
Historically used by early humans for making stone tools, arrowheads, and blades due to its sharp conchoidal fracture. Today used occasionally in abrasives or decorative landscaping.
Geological facts
Chert breaks with extremely sharp edges, making it one of the premier materials for prehistoric tool-making across the globe. Varieties of chert include flint and jasper.
Field identification & locations
Easily identified in the field by its smooth, waxy luster, conchoidal fracture patterns, and hardness that easily scratches glass. Commonly found within limestone or chalk formations worldwide.
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