Rock Identifier
Quartz (Milky Quartz) (Silicon Dioxide (SiO2)) — mineral
mineral

Quartz (Milky Quartz)

Silicon Dioxide (SiO2)

Hardness: 7.0 Mohs; Color: Milky white to translucent; Luster: Vitreous to greasy; Crystal Structure: Hexagonal; Cleavage: None/Conchoidal fracture; Specific Gravity: 2.65

Hardness
7
Color
Milky white to translucent
Luster
Vitreous to greasy
Identified More mineral
Explore Quartz (Milky Quartz) in the encyclopedia →

Identify your own rocks.

Get a report just like this from any photo, free.

Physical properties

Hardness: 7.0 Mohs; Color: Milky white to translucent; Luster: Vitreous to greasy; Crystal Structure: Hexagonal; Cleavage: None/Conchoidal fracture; Specific Gravity: 2.65

Formation & geological history

Formed through hydrothermal processes, crystallization from magma, or within metamorphic rocks. It is found across all geological eras in various environments.

Uses & applications

Used in glass manufacturing, electronics (due to piezoelectric properties), construction aggregates, as semi-precious gemstones, and in abrasive applications.

Geological facts

Quartz is the second most abundant mineral in Earth's continental crust. Milky quartz gets its appearance from tiny fluid inclusions of gas or liquid trapped during crystal growth.

Field identification & locations

Identify in the field by its hardness (it scratches glass) and lack of cleavage. It is found globally, particularly in vein deposits and pegmatites.