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: Trigonal/Hexagonal; Cleavage: None (conchoidal fracture); Specific Gravity: 2.65
Formation & Geological History
Formed from the crystallization of silica-rich hydrothermal fluids in veins or as a major constituent in igneous rocks like granite. Its white color comes from minute fluid inclusions of gas or liquid trapped during crystal growth.
Uses & Applications
Used in the glass and ceramics industry, as a flux in metallurgy, and as decorative stone in landscaping. High-purity quartz is used in electronics and semiconductors.
Geological Facts
Quartz is the second most abundant mineral in Earth's continental crust. Milky quartz specifically is the most common variety found in nature and can be found in mountain ranges worldwide.
Field Identification & Locations
Identify by its hardness (it will scratch glass and steel), lack of cleavage, and waxy or glassy luster. Found globally in almost every geological environment, often as prominent white veins in darker host rock.
Identified on: 4/14/2026
Mode: Standard