Milky Quartz
Silicon Dioxide (SiO2)
Rock Type: mineral

Physical Properties
Hardness: 7 on Mohs scale; Color: Milky white to cream; 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 as a component of igneous and metamorphic rocks. Frequently found as water-worn pebbles in riverbeds or beaches.
Uses & Applications
Used as a gemstone (cabochons), in glass making, as a source of silicon for electronics, and in decorative landscaping or aquarium gravel.
Geological Facts
The milky white color is caused by tiny inclusions of gas or liquid trapped during crystal growth. It is one of the most common minerals on the Earth's crust.
Field Identification & Locations
Identify in the field by its hardness (scratches glass), white color, and lack of cleavage. Often found in riverbeds, mountain veins, and glacial deposits globally.
Identified on: 5/20/2026
Mode: Standard