Rock Identifier
Quartz Nut (SiO2 (Silicon Dioxide)) — mineral health
mineral health

Quartz Nut

SiO2 (Silicon Dioxide)

Hardness: 7 Mohs; Color: White to tan with iron staining; Luster: Vitreous to waxy; Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture).

Hardness
7 Mohs
Color
White to tan with iron staining
Luster
Vitreous to waxy
Identified More mineral health
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Physical properties

Hardness: 7 Mohs; Color: White to tan with iron staining; Luster: Vitreous to waxy; Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture).

Formation & geological history

Forms through the cooling of silica-rich magma or from hydrothermal veins. Often found as weather-worn pebbles in alluvial deposits or riverbeds.

Uses & applications

Industrial uses include electronics, glass making, and abrasives. As a rough specimen, it serves as an educational tool for mineral identification.

Geological facts

Quartz is the second most abundant mineral in Earth's continental crust. Its name comes from the German word 'Quarz', which had its origins in Slavic and West Slavonic words meaning 'hard'.

Field identification & locations

Identified in the field by its hardness (it will scratch glass) and lack of cleavage. Common in riverbeds, mountains, and desert pavement worldwide.