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

Clear Quartz

Silicon dioxide (SiO2)

Hardness: 7 on the Mohs scale. Color: Colorless/Transparent. Luster: Vitreous. Crystal Structure: Hexagonal (trigonal). Cleavage: None (conchoidal fracture). Specific Gravity: 2.65.

Hardness
7 on the Mohs scale
Color
Colorless/Transparent
Luster
Vitreous
Identified More mineral
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Physical properties

Hardness: 7 on the Mohs scale. Color: Colorless/Transparent. Luster: Vitreous. Crystal Structure: Hexagonal (trigonal). Cleavage: None (conchoidal fracture). Specific Gravity: 2.65.

Formation & geological history

Formed in various geological environments, most commonly in igneous rocks like granite pegmatites and metamorphic rocks. This specimen likely originated from the Brazil crystalline shield which is billions of years old.

Uses & applications

Used in electronics for its piezoelectric properties, glass manufacturing, as a gemstone in jewelry, and widely collected as metaphysical or decorative specimens.

Geological facts

Quartz is the second most abundant mineral in Earth's continental crust. The location provided (Minas Gerais, Brazil) is world-famous for producing some of the highest quality quartz crystals on Earth.

Field identification & locations

Identify by its hardness (scratches glass), lack of cleavage, and transparent appearance. Minas Gerais is a primary global source for this mineral.