Rock Identifier
Chert (specifically Flint or Jasper variant) (Microcrystalline Quartz (SiO2)) — sedimentary
sedimentary

Chert (specifically Flint or Jasper variant)

Microcrystalline Quartz (SiO2)

Hardness: 7 on Mohs scale; Color: Brown, tan, and dark translucent patches; Luster: Waxy to vitreous; Crystal Structure: Trigonal (cryptocrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.

Hardness
7 on Mohs scale
Color
Brown, tan, and dark translucent patches
Luster
Waxy to vitreous
Identified More sedimentary
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Physical properties

Hardness: 7 on Mohs scale; Color: Brown, tan, and dark translucent patches; Luster: Waxy to vitreous; Crystal Structure: Trigonal (cryptocrystalline); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.

Formation & geological history

Formed through the accumulation of silica-rich organic or chemical deposits in sedimentary environments. Often found as nodules in limestone or chalk beds. This specimen appears to have water-worn or weathered cortex.

Uses & applications

Historically used for stone tools (knapping) and fire-starting. Currently used as an abrasive, in decorative landscaping, or as a semi-precious gemstone when polished.

Geological facts

Chert was one of the most important lithic materials for prehistoric humans due to its predictable conchoidal fracturing, which allows for the creation of razor-sharp edges.

Field identification & locations

Identify by its waxy luster, hardness (can scratch glass), and shell-like (conchoidal) fractures on broken surfaces. Commonly found in riverbeds, gravel pits, and eroding out of limestone outcrops.