Chert (Iron-stained)
Microcrystalline Quartz (SiO2)
Rock Type: sedimentary

Physical Properties
Hardness: 6.5-7 on Mohs scale. Color: Tan, yellow-brown due to iron oxide staining. Luster: Dull to waxy. Structure: Cryptocrystalline. Cleavage: None (conchoidal fracture). Specific Gravity: 2.6-2.7.
Formation & Geological History
Formed through the accumulation of silica-rich organic remains (like diatoms or radiolarians) or inorganic precipitation from silica-rich fluids within sedimentary rock layers, often limestone or dolostone.
Uses & Applications
Historically used for stone tools (arrowheads/scrapers) due to conchoidal fracturing. Modernly used in road construction, landscaping, and as a polishing abrasive.
Geological Facts
Chert was one of the first materials used by early humans for fire-starting and tool-making because it produces sharp edges and sparks when struck against steel or iron pyrites.
Field Identification & Locations
Identify by its extreme hardness (cannot be scratched by a steel blade) and its smooth, shell-like (conchoidal) fracture surfaces. Commonly found in riverbeds or within limestone outcrops.
Identified on: 4/18/2026
Mode: Standard