Milky Quartz
Silicon Dioxide (SiO2)
Rock Type: mineral

Physical Properties
Hardness: 7 on Mohs scale; Color: Milky white to translucent; Luster: Vitreous to greasy; Crystal Structure: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & Geological History
Formed from silica-rich hydrothermal fluids cooling in veins or from the crystallization of pegmatites. It is the most common variety of crystalline quartz.
Uses & Applications
Used in electronics as a source of high-purity silica, as an abrasive, in glassmaking, and frequently in decorative landscaping or as affordable collector specimens.
Geological Facts
The milky white color is caused by tiny inclusions of gas or liquid trapped during the crystal's growth. It is often found associated with gold in hydrothermal veins.
Field Identification & Locations
Identify in the field by its hardness (will scratch glass easily), lack of cleavage, and white color. It is omnipresent in granite-rich terrains and riverbeds globally.
Identified on: 5/13/2026
Mode: Standard