Rock Identifier
Clear Quartz (Silicon dioxide (SiO2)) — mineral
mineral

Clear Quartz

Silicon dioxide (SiO2)

Hardness: 7 (Mohs scale), Color: Colorless to white, Luster: Vitreous (glassy), Crystal structure: Trigonal/Hexagonal, Cleavage: None (conchoidal fracture), Specific gravity: 2.65

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Physical properties

Hardness: 7 (Mohs scale), Color: Colorless to white, Luster: Vitreous (glassy), Crystal structure: Trigonal/Hexagonal, Cleavage: None (conchoidal fracture), Specific gravity: 2.65

Formation & geological history

Formed from cooling magma or hydrothermally in veins and geodes. It is found in all types of geological environments (igneous, metamorphic, and sedimentary) and can be multi-billion years old.

Uses & applications

Used in electronics (oscillators), glassmaking, precision instruments, jewelry, and as a popular collector's specimen.

Geological facts

Also known as 'Rock Crystal.' It is one of the most abundant minerals on Earth's crust and exhibits piezoelectric properties, meaning it can generate an electric charge in response to applied mechanical stress.

Field identification & locations

Identify by its hardness (scratches glass), lack of cleavage, and transparent appearance. Commonly found in quartz veins or as pebbles in riverbeds.