Milky Quartz
Silicon dioxide (SiO2)
Rock Type: mineral

Physical Properties
Hardness: 7 (Mohs scale), Color: White to cloudy (due to fluid/gas inclusions), 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 or within pegmatites. It is commonly found in igneous intrusions and metamorphic veins. It can be found in terrains ranging from Precambrian to Cenozoic.
Uses & Applications
Used in the production of glass, ceramics, and abrasives. In electronics, it's used for its piezoelectric properties. It is also used as decorative stone, in landscaping, and as a collector's mineral.
Geological Facts
Milky quartz is the most common variety of crystalline quartz. The white 'milky' color is caused by millions of tiny bubbles of gas or liquid trapped during the crystal's growth.
Field Identification & Locations
Identify in the field by its hardness (scratches glass/steel), lack of cleavage, and characteristic waxy/glassy appearance. It is found globally in mountainous regions and riverbeds.
Identified on: 4/20/2026
Mode: Standard