Rock Identifier
Quartz (Chert/Quartzite variant) (Silicon Dioxide (SiO2)) — mineral
mineral

Quartz (Chert/Quartzite variant)

Silicon Dioxide (SiO2)

Hardness: 7 (Mohs scale); Color: Tan, brown, and greyish; Luster: Vitreous to waxy; Crystal structure: Hexagonal (though massive/microcrystalline in this form); Specific gravity: approx. 2.65

Hardness
7 (Mohs scale)
Color
Tan, brown, and greyish
Luster
Vitreous to waxy
Identified More mineral
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Physical properties

Hardness: 7 (Mohs scale); Color: Tan, brown, and greyish; Luster: Vitreous to waxy; Crystal structure: Hexagonal (though massive/microcrystalline in this form); Specific gravity: approx. 2.65

Formation & geological history

Formed primarily through the chemical precipitation of silica or from the metamorphism of quartz-rich sandstone. Most commonly found in sedimentary sequences or as veins in various rock types.

Uses & applications

Largely used as an abrasive, in glass manufacturing, or as construction aggregate. Historically used for making tools like scrapers and arrowheads due to its conchoidal fracture.

Geological facts

Quartz is the second most abundant mineral in the Earth's continental crust. It is highly resistant to both chemical and physical weathering.

Field identification & locations

Check for hardness by seeing if it scratches glass. Look for the characteristic conchoidal fracture (curved, shell-like breaks) and a lack of cleavage. Common in riverbeds and gravel pits.