
sedimentary
Chert (Iron-stained)
Microcrystalline or Cryptocrystalline Quartz (SiO2)
Hardness: 7 (Mohs scale); Color: Dark brown to black with iron-oxide staining; Luster: Waxy to dull; Crystal structure: Hexagonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.65
- Hardness
- 7 (Mohs scale)
- Color
- Dark brown to black with iron-oxide staining
- Luster
- Waxy to dull
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Physical properties
Hardness: 7 (Mohs scale); Color: Dark brown to black with iron-oxide staining; Luster: Waxy to dull; Crystal structure: Hexagonal (microcrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.65
Formation & geological history
Formed through the accumulation of silica-rich organic remains (diatoms, radiolarians) or chemical precipitation from groundwater within sedimentary layers. This specific piece shows significant weather-induced iron oxidation.
Uses & applications
Historically used for stone tools and starting fires (flint); currently used in road construction, as an abrasive, and by lapidary hobbyists for tumbling or jewelry.
Geological facts
Because of its high silica content and density, chert was a primary material for prehistoric arrowheads and scrapers. It can range in color from white to pitch black depending on impurities.
Field identification & locations
Identify in the field by its hardness (it will scratch glass and steel) and its shell-like conchoidal fracture patterns. Found globally in limestone beds or as stream gravel.
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