
sedimentary
Chert (specifically Banded Chert)
Microcrystalline or Cryptocrystalline Quartz (SiO2)
Hardness: 7 on Mohs scale; Color: typically gray, tan, or brown with distinct lighter/darker bands; Luster: waxy to dull; Structure: microcrystalline (no visible crystals); Cleavage: none (fractures conchoidally); Specific Gravity: 2.65.
- Hardness
- 7 on Mohs scale
- Luster
- waxy to dull
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Physical properties
Hardness: 7 on Mohs scale; Color: typically gray, tan, or brown with distinct lighter/darker bands; Luster: waxy to dull; Structure: microcrystalline (no visible crystals); Cleavage: none (fractures conchoidally); Specific Gravity: 2.65.
Formation & geological history
Formed from the accumulation of silica-rich organic remains (like radiolaria or diatoms) or chemical precipitation from silica-rich fluids within limestone or chalk beds. Often Paleozoic or Mesozoic in age.
Uses & applications
Historically used for stone tools (arrowheads, scrapers) due to its sharp edges. Modernly used in construction aggregate, road surfacing, and as a polishing media in rock tumblers.
Geological facts
Because it breaks with a conchoidal fracture like glass, it was one of the most important minerals for prehistoric survival. It is so chemically stable that it often remains intact long after the surrounding limestone has weathered away.
Field identification & locations
Identify in the field by its hardness (it will scratch glass or steel) and its smooth, shell-like fracture surfaces. It often feels 'slicker' than surrounding limestone. Commonly found in riverbeds or eroding out of limestone cliffs.
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