Chert (Flint)
Microcrystalline Quartz (SiO2)
Rock Type: sedimentary

Physical Properties
Hardness: 7 on Mohs scale; Color: Gray, tan, or white with waxy luster; Crystal Structure: Cryptocrystalline; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & Geological History
Formed through the accumulation of silica-rich organic remains (like radiolarians or diatoms) or chemical precipitation in marine environments. Often found as nodules in limestone or chalk beds.
Uses & Applications
Historically used for stone tools and starting fires (sparking). Modern uses include road surfacing, abrasives, and as a component in jewelry (jasper/agate varieties).
Geological Facts
Chert was one of the most important minerals for early humans because its conchoidal fracture produces extremely sharp edges, ideal for arrowheads and scrapers.
Field Identification & Locations
Identify by its waxy appearance, extreme hardness (scratches glass), and shell-like (conchoidal) breakage patterns. Found globally in sedimentary basins.
Identified on: 4/29/2026
Mode: Standard