sedimentary

Chert (Blue-Gray Chert)

Microcrystalline quartz (SiO2)

Hardness: 6.5-7 on Mohs scale; Color: Grayish-blue with brown iron staining; Luster: Waxy to vitreous; Crystal structure: Trigonal (cryptocrystalline); Cleavage: None (conchoidal fracture); Specific gravity: 2.6-2.7

Hardness: 6
Color: Grayish-blue with brown iron staining
Luster: Waxy to vitreous

Identified April 19, 2026More sedimentary →

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Physical properties

Formation & geological history

Formed through the accumulation of silica-rich organic remains (like diatoms or radiolarians) or inorganic precipitation from silica-saturated water in sedimentary basins. It is often found within limestone or chalk formations.

Uses & applications

Historically used for stone tools and arrowheads; currently used as garden decoration, road base, and as a semi-precious gemstone for cabochons if the color is unique.

Geological facts

Chert is so hard that it can strike sparks against steel, making it a primary material for flintlock firearms and primitive fire-starting. This specific grayish-blue variety is often affectionately called 'blue flint' by collectors.

Field identification & locations

Identify in the field by its smooth, waxy feel and circular 'conchoidal' fracture patterns (like broken glass). It will scratch common glass and cannot be scratched by a steel knife. Commonly found in riverbeds and limestone outcrops.

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Sandstone or Siltstone

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Chert Breccia

Brecciated Chert (Microcrystalline Silica)

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Sandstone Grain

Clastic Sedimentary Rock Grain (SiO2 dominated)

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Shale or Slaty Mudstone

Argillaceous sedimentary rock

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Sandstone

Arenite

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