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 and cavities within igneous, metamorphic, and sedimentary rocks. Its cloudy white color is caused by microscopic fluid inclusions trapped during growth.
Uses & Applications
Used as a source of silicon for semiconductors, manufacturing of glass and ceramics, as an abrasive, in construction as aggregate, and frequently used in lapidary for decorative stones.
Geological Facts
Milky Quartz is one of the most common varieties of crystalline quartz on Earth. The white opacity is due to tiny bubbles of gas or liquid that were trapped when the crystal was forming millions of years ago.
Field Identification & Locations
Identify in the field by its hardness (will scratch glass), lack of cleavage, and white 'milky' appearance. It is found globally, particularly in mountainous regions and riverbeds.
Identified on: 4/30/2026
Mode: Standard