Milky Quartz
Quartz (Silicon Dioxide, SiO2)
Rock Type: mineral

Physical Properties
Hardness: 7 on Mohs scale; Color: Opaque white; Luster: Vitreous to greasy; Crystal structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific gravity: 2.65
Formation & Geological History
Formed through the crystallization of silica-rich hydrothermal veins or from the cooling of magma in igneous rocks. The milky color is caused by tiny inclusions of gas or liquid trapped during crystal growth.
Uses & Applications
Used in glassmaking, as an abrasive, in the production of silicon for electronics, as landscaping stone, and occasionally in jewelry or as a decorative collector's item.
Geological Facts
Milky quartz is the most common variety of crystalline quartz. Historically, it was used by many indigenous cultures to create sharp stone tools and spearheads when flint was unavailable.
Field Identification & Locations
Identify in the field by its ability to scratch glass, its milky white opacity, and the absence of cleavage planes. Found globally in almost all geological environments.
Identified on: 4/26/2026
Mode: Standard