Rock Identifier
Quartz (specifically Clear Quartz or Rock Crystal) (Silicon Dioxide (SiO2)) — mineral
mineral

Quartz (specifically Clear Quartz or Rock Crystal)

Silicon Dioxide (SiO2)

Hardness: 7 on Mohs scale; Color: Colorless to faint yellow/smoky; Luster: Vitreous (glassy); Crystal Structure: Hexagonal/Trigonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.

Hardness
7 on Mohs scale
Color
Colorless to faint yellow/smoky
Luster
Vitreous (glassy)
Identified More mineral

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Physical properties

Hardness: 7 on Mohs scale; Color: Colorless to faint yellow/smoky; Luster: Vitreous (glassy); Crystal Structure: Hexagonal/Trigonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.

Formation & geological history

Formed from cooling magma or hydrothermal veins. It is found in all types of geological environments and can be found in rocks from the Precambrian era to the present.

Uses & applications

Extensively used in electronics (oscillators), glass manufacturing, abrasives, construction sand, and as a gemstone in jewelry and metaphysical collecting.

Geological facts

Quartz is the second most abundant mineral in Earth's continental crust. It is piezoelectric, meaning it generates an electric charge when mechanical pressure is applied.

Field identification & locations

Identify in the field by its glass-like appearance, inability to be scratched by a steel knife, and lacks cleavage (it breaks into curved, shell-like shards). Common in riverbeds and mountainous regions globally.