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

Physical Properties
Hardness: 7 on Mohs scale; Color: Opaque white to translucent; Luster: Vitreous to greasy; Crystal Structure: Hexagonal (trigonal); Cleavage: None (conchoidal fracture); Specific Gravity: 2.65.
Formation & Geological History
Formed through hydrothermal processes or during the final stages of cooling in igneous magma bodies. It is found in veins and as a primary constituent of granites and quartzites across almost all geological ages.
Uses & Applications
Used in electronics for its piezoelectric properties, as an abrasive, in glass manufacturing, as an aggregate in construction, and in metaphysical or ornamental jewelry.
Geological Facts
Milky Quartz gets its white color from tiny fluid inclusions of gas or liquid trapped during the crystal's growth. It is the most common variety of crystalline quartz.
Field Identification & Locations
Identify by its hardness (it will scratch glass), its lack of cleavage, and its distinctive milky appearance. It is ubiquitous in mountainous regions and riverbeds worldwide.
Identified on: 4/19/2026
Mode: Standard